GERM Reservoir Database
Development and Maintenance by the EarthRef.org Database Team

GERM Database Search Results        
Reservoir Z Element Value Median SD Low High N Unit Info Reference Source(s)
Angra dos Reis Angrite 47 Ag 18           ppb Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Laul et al. 1972
Angra dos Reis Angrite 79 Au 7.17           ppb Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Laul et al. 1972
Angra dos Reis Angrite 83 Bi 2.4           ppb Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Laul et al. 1972
Angra dos Reis Angrite 35 Br 413           ppb Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Laul et al. 1972
Angra dos Reis Angrite 27 Co 20.4           ppm Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Laul et al. 1972
Angra dos Reis Angrite 55 Cs 1.9           ppb Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Laul et al. 1972
Angra dos Reis Angrite 29 Cu 1100           ppm Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Value suspected of contamination. Laul et al. 1972
Angra dos Reis Angrite 31 Ga 0.36           ppm Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Laul et al. 1972
Angra dos Reis Angrite 49 In 1.43           ppb Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Laul et al. 1972
Angra dos Reis Angrite 77 Ir 2.6           ppb Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Laul et al. 1972
Angra dos Reis Angrite 81 Tl 0.86           ppb Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Laul et al. 1972
Angra dos Reis Angrite 30 Zn 2.1           ppm Elemental abundance of the Angra dos Reis meteorite. Classified as an Angrite, the sample itself consists of a thin slice of material most likely made with a cutoff wheel. However, the high abundance of Cu in the sample indicates that the sample was contaminated from the wheel used to make the slice of material. Laul et al. 1972
Bereba Eucrite 47 Ag 98           ppb Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 79 Au 2.82           ppb Laul et al. 1972
Bereba Eucrite 79 Au 2.82           ppb Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 83 Bi 7           ppb Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 35 Br 34           ppb Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 48 Cd 8.7           ppb Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 27 Co 4.7           ppm Laul et al. 1972
Bereba Eucrite 27 Co 4.7           ppm Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 55 Cs 7.9           ppb Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 29 Cu 3.78           ppm Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 29 Cu 3.78           ppm Laul et al. 1972
Bereba Eucrite 31 Ga 1.45           ppm Laul et al. 1972
Bereba Eucrite 31 Ga 1.45           ppm Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 49 In 0.94           ppb Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation.1 Laul et al. 1972
Bereba Eucrite 77 Ir 0.7           ppb Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 77 Ir 0.7           ppb Laul et al. 1972
Bereba Eucrite 34 Se 329           ppb Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 34 Se 329           ppb Laul et al. 1972
Bereba Eucrite 81 Tl 0.31           ppb Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bereba Eucrite 30 Zn 1.3           ppm Elemental abundance of the B¿r¿ba meteorite. Sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 47 Ag 19           ppb Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 79 Au 3.94           ppb Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 83 Bi 2.3           ppb Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 35 Br 374           ppb Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 48 Cd 1.8           ppb Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 27 Co 14           ppm Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 55 Cs 7.8           ppb Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 29 Cu 0.77           ppm Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 31 Ga 1.34           ppm Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 49 In 2.73           ppb Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 77 Ir 5.74           ppb Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 34 Se 118           ppb Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 81 Tl 0.57           ppb Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Bialystok Howardite 30 Zn 1.4           ppm Elemental abundance of the Bialystok meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 47 Ag 30           ppb Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 79 Au 6.74           ppb Laul et al. 1972
Constantinople Eucrite 79 Au 6.74           ppb Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 83 Bi 0.77           ppb Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 35 Br 26           ppb Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 48 Cd 3.5           ppb Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 27 Co 7.4           ppm Laul et al. 1972
Constantinople Eucrite 27 Co 7.4           ppm Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 55 Cs 12.1           ppb Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 29 Cu 1.88           ppm Laul et al. 1972
Constantinople Eucrite 29 Cu 1.88           ppm Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 31 Ga 1.51           ppm Laul et al. 1972
Constantinople Eucrite 31 Ga 1.51           ppm Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 49 In 1.82           ppb Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 77 Ir 0.31           ppb Laul et al. 1972
Constantinople Eucrite 77 Ir 0.31           ppb Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 34 Se 396           ppb Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 34 Se 396           ppb Laul et al. 1972
Constantinople Eucrite 81 Tl 1.97           ppb Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Constantinople Eucrite 30 Zn 20           ppm Elemental abundance of the Constantinople meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 47 Ag 17           ppb Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 79 Au 4.13           ppb Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 83 Bi 180           ppb Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 35 Br 66           ppb Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 27 Co 21.8           ppm Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 55 Cs 6.3           ppb Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 29 Cu 18.2           ppm Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 31 Ga 0.72           ppm Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 49 In 2.35           ppb Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 77 Ir 3.5           ppb Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 81 Tl 0.51           ppb Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Frankfort Howardite 30 Zn 1.6           ppm Elemental abundance of the Frankfort meteorite. Classified as a Howardite, the sample itself consists of one or several chips between 500-300 mg. No cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 47 Ag 37           ppb Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 79 Au 3.93           ppb Laul et al. 1972
Jonzac Eucrite 79 Au 3.93           ppb Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 83 Bi 5.3           ppb Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 35 Br 164           ppb Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 48 Cd 3           ppb Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 27 Co 9.3           ppm Laul et al. 1972
Jonzac Eucrite 27 Co 9.3           ppm Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 55 Cs 15.7           ppb Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 29 Cu 8.52           ppm Laul et al. 1972
Jonzac Eucrite 29 Cu 8.52           ppm Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 31 Ga 1.45           ppm Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 31 Ga 1.45           ppm Laul et al. 1972
Jonzac Eucrite 49 In 1.23           ppb Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 77 Ir 0.46           ppb Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 77 Ir 0.46           ppb Laul et al. 1972
Jonzac Eucrite 34 Se 164           ppb Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 34 Se 164           ppb Laul et al. 1972
Jonzac Eucrite 81 Tl 1.16           ppb Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Jonzac Eucrite 30 Zn 6.3           ppm Elemental abundance of the Jonzac meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Juvinas Eucrite 47 Ag 21           ppb Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Juvinas Eucrite 79 Au 3.82           ppb Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Juvinas Eucrite 79 Au 3.82           ppb Laul et al. 1972
Juvinas Eucrite 83 Bi 5           ppb Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Juvinas Eucrite 35 Br 146           ppb Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Juvinas Eucrite 27 Co 6.5           ppm Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Juvinas Eucrite 27 Co 6.5           ppm Laul et al. 1972
Juvinas Eucrite 55 Cs 8.2           ppb Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Juvinas Eucrite 29 Cu 2.44           ppm Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Juvinas Eucrite 29 Cu 2.44           ppm Laul et al. 1972
Juvinas Eucrite 31 Ga 1.48           ppm Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Juvinas Eucrite 31 Ga 1.48           ppm Laul et al. 1972
Juvinas Eucrite 49 In 1.61           ppb Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Juvinas Eucrite 77 Ir 4.1           ppb Suspected of contamination. Laul et al. 1972
Juvinas Eucrite 77 Ir 4.1           ppb Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Suspected of contamination. Laul et al. 1972
Juvinas Eucrite 81 Tl 0.75           ppb Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Juvinas Eucrite 30 Zn 2.5           ppm Elemental abundance of the Juvinas meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Kapoeta Howardite 47 Ag 7.3           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 47 Ag 3.1           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 79 Au 3.71           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 79 Au 2.15           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 83 Bi 4.56           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 83 Bi 1.52           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 35 Br 40           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 35 Br 139           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 48 Cd 7.6           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 48 Cd 1.6           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 27 Co 21.6           ppm Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 27 Co 23.6           ppm Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 55 Cs 2.3           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 55 Cs 8.6           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 29 Cu 3.71           ppm Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 29 Cu 2.44           ppm Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 31 Ga 1.1           ppm Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 31 Ga 1.3           ppm Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 49 In 3.13           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 49 In 1.67           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 81 Tl 27           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Value suspect of contamination. Laul et al. 1972
Kapoeta Howardite 81 Tl 52           ppb Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Value suspect of contamination. Laul et al. 1972
Kapoeta Howardite 30 Zn 0.47           ppm Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of light material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Kapoeta Howardite 30 Zn 0.35           ppm Elemental abundance of the Kapoeta meteorite. Classified as a Howardite, the sample itself consists of dark material from the gas-rich, brecciated meteorite were obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Lafayette Nakhlite 47 Ag 58           ppb Elemental abundance of the Lafayette meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Lafayette Nakhlite 79 Au 21           ppb Elemental abundance of the Lafayette meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Lafayette Nakhlite 83 Bi 5.64           ppb Elemental abundance of the Lafayette meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Lafayette Nakhlite 48 Cd 92           ppb Elemental abundance of the Lafayette meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Lafayette Nakhlite 55 Cs 288           ppb Elemental abundance of the Lafayette meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Lafayette Nakhlite 49 In 20.3           ppb Elemental abundance of the Lafayette meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Lafayette Nakhlite 77 Ir 0.13           ppb Elemental abundance of the Lafayette meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Lafayette Nakhlite 37 Rb 2.4           ppm Elemental abundance of the Lafayette meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Lafayette Nakhlite 34 Se 88           ppb Elemental abundance of the Lafayette meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Lafayette Nakhlite 81 Tl 7.2           ppb Elemental abundance of the Lafayette meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Lafayette Nakhlite 30 Zn 71           ppm Elemental abundance of the Lafayette meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 47 Ag 214           ppb Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 79 Au 11.4           ppb Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 83 Bi 3.8           ppb Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 35 Br 84           ppb Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 48 Cd 88           ppb Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 27 Co 35           ppm Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 55 Cs 28           ppb Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 29 Cu 8.4           ppm Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 31 Ga 1.08           ppm Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 49 In 7.63           ppb Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 77 Ir 31           ppb Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 34 Se 556           ppb Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 81 Tl 4.3           ppb Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Molteno Howardite 30 Zn 30           ppm Elemental abundance of the Molteno meteorite. Classified as a Howardite, the sample itself consists of light material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 47 Ag 40           ppb Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 79 Au 0.55           ppb Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 83 Bi 0.5           ppb Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 35 Br 4370           ppb Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 48 Cd 71           ppb Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 27 Co 81           ppm Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 55 Cs 287           ppb Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 29 Cu 5.03           ppm Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 31 Ga 2.7           ppm Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 49 In 24.4           ppb Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 77 Ir 17           ppb Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 37 Rb 2.8           ppm Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 81 Tl 3.1           ppb Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Nakhla Nakhlite 30 Zn 42           ppm Elemental abundance of the Nakhla meteorite. Classified as a Nakhlite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Pesyanoe Aubrite 47 Ag 74           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of dark material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 47 Ag 13           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of light material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 79 Au 6.49           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of light material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 79 Au 6.48           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of dark material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 83 Bi 2.3           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of light material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 83 Bi 4.5           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of dark material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 35 Br 260           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of light material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 35 Br 280           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of dark material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 27 Co 2.4           ppm Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of dark material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 27 Co 14           ppm Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of light material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 31 Ga 0.056           ppm Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of dark material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 49 In 0.51           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of light material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 49 In 0.53           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of dark material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 77 Ir 5.15           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of light material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 77 Ir 1.34           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of dark material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 34 Se 1780           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of dark material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 34 Se 2090           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of light material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 81 Tl 90           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of light material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Value suspect of contamination. Laul et al. 1972
Pesyanoe Aubrite 81 Tl 2200           ppb Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of dark material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Value suspect of contamination. Laul et al. 1972
Pesyanoe Aubrite 30 Zn 1.6           ppm Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of light material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Pesyanoe Aubrite 30 Zn 4.5           ppm Elemental abundance of the Pesyanoe meteorite. Classified as an Angrite, the sample itself consists of dark material from the gas-rich, brecciated meteorite which was obtained by Dr. Brian Mason (U.S. National Museum). Laul et al. 1972
Sera de Mage Eucrite 47 Ag 3.3           ppb Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 79 Au 1.75           ppb Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 79 Au 53           ppb Laul et al. 1972
Sera de Mage Eucrite 83 Bi 2.4           ppb Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 35 Br 45           ppb Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 48 Cd 5.3           ppb Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 27 Co 6.5           ppm Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 55 Cs 2.1           ppb Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 29 Cu 2.32           ppm Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 31 Ga 1.42           ppm Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 49 In 0.73           ppb Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 77 Ir 53           ppb Suspected of contamination. Laul et al. 1972
Sera de Mage Eucrite 77 Ir 53           ppb Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. The Ir value of this sample is suspiciously high, which suggests contamination during handling. Laul et al. 1972
Sera de Mage Eucrite 34 Se 78           ppb Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 81 Tl 0.12           ppb Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Sera de Mage Eucrite 30 Zn 0.78           ppm Elemental abundance of the Serra de Mag¿ meteorite. Classified as an unbrecciated eucrite, the sample used was a powder which had been reconstituted in the original proportions from magnetically separated pyroxene and feldspar fractions. Laul et al. 1972
Shergotty Shergottite 47 Ag 263           ppb Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 79 Au 88           ppb Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 83 Bi 3.7           ppb Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 35 Br 1070           ppb Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 48 Cd 44           ppb Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 27 Co 63           ppm Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 55 Cs 380           ppb Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 29 Cu 11.9           ppm Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 31 Ga 13.9           ppm Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 49 In 31.3           ppb Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 77 Ir 1.55           ppb Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 37 Rb 6.1           ppm Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 34 Se 242           ppb Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 81 Tl 13.4           ppb Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Shergotty Shergottite 30 Zn 76           ppm Elemental abundance of the Shergotty meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Sioux County Eucrite 47 Ag 5.5           ppb Elemental abundance of the Sioux County meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Sioux County Eucrite 79 Au 0.33           ppb Laul et al. 1972
Sioux County Eucrite 79 Au 0.33           ppb Elemental abundance of the Sioux County meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Sioux County Eucrite 83 Bi 0.37           ppb Elemental abundance of the Sioux County meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Sioux County Eucrite 27 Co 4.3           ppm Elemental abundance of the Sioux County meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Sioux County Eucrite 27 Co 4.3           ppm Laul et al. 1972
Sioux County Eucrite 55 Cs 7.9           ppb Elemental abundance of the Sioux County meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Sioux County Eucrite 29 Cu 0.94           ppm Elemental abundance of the Sioux County meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Sioux County Eucrite 29 Cu 0.94           ppm Laul et al. 1972
Sioux County Eucrite 31 Ga 1.26           ppm Elemental abundance of the Sioux County meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Sioux County Eucrite 31 Ga 1.26           ppm Laul et al. 1972
Sioux County Eucrite 49 In 0.52           ppb Elemental abundance of the Sioux County meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Sioux County Eucrite 81 Tl 0.2           ppb Elemental abundance of the Sioux County meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Sioux County Eucrite 30 Zn 1.3           ppm Elemental abundance of the Sioux County meteorite. Classified as a eucrite the sample consisted of one or several chips between 500-300 mg, and no cleaning was attempted before irradiation. Laul et al. 1972
Stannern Trend Eucrites 47 Ag 40           ppb Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 47 Ag 2100           ppb Elemental abundance of the Stannern meteorite sample 1. Classified as a eucrite the sample was taken from a region of the meteorite that was stained yellow. This sample turned out to have higher concentrations of 10 trace elements, upwards of two orders of magnitude, than other eucrites. Laul et al. 1972
Stannern Trend Eucrites 79 Au 78.4           ppb Laul et al. 1972
Stannern Trend Eucrites 79 Au 24.5           ppb Laul et al. 1972
Stannern Trend Eucrites 79 Au 78.4           ppb Elemental abundance of the Stannern meteorite sample 1. Classified as a eucrite the sample was taken from a region of the meteorite that was stained yellow. This sample turned out to have higher concentrations of 10 trace elements, upwards of two orders of magnitude, than other eucrites. Laul et al. 1972
Stannern Trend Eucrites 79 Au 24.5           ppb Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 83 Bi 318           ppb Elemental abundance of the Stannern meteorite sample 1. Classified as a eucrite the sample was taken from a region of the meteorite that was stained yellow. This sample turned out to have higher concentrations of 10 trace elements, upwards of two orders of magnitude, than other eucrites. Laul et al. 1972
Stannern Trend Eucrites 83 Bi 6.4           ppb Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 35 Br 290           ppb Elemental abundance of the Stannern meteorite sample 1. Classified as a eucrite the sample was taken from a region of the meteorite that was stained yellow. This sample turned out to have higher concentrations of 10 trace elements, upwards of two orders of magnitude, than other eucrites. Laul et al. 1972
Stannern Trend Eucrites 35 Br 61           ppb Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 48 Cd 1.7           ppb Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 27 Co 7.3           ppm Laul et al. 1972
Stannern Trend Eucrites 27 Co 14.7           ppm Elemental abundance of the Stannern meteorite sample 1. Classified as a eucrite the sample was taken from a region of the meteorite that was stained yellow. This sample turned out to have higher concentrations of 10 trace elements, upwards of two orders of magnitude, than other eucrites. Laul et al. 1972
Stannern Trend Eucrites 27 Co 14.7           ppm Laul et al. 1972
Stannern Trend Eucrites 27 Co 7.3           ppm Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 55 Cs 43.5           ppb Elemental abundance of the Stannern meteorite sample 1. Classified as a eucrite the sample was taken from a region of the meteorite that was stained yellow. This sample turned out to have higher concentrations of 10 trace elements, upwards of two orders of magnitude, than other eucrites. Laul et al. 1972
Stannern Trend Eucrites 55 Cs 16.2           ppb Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 29 Cu 1.04           ppm Laul et al. 1972
Stannern Trend Eucrites 29 Cu 20.7           ppm Laul et al. 1972
Stannern Trend Eucrites 29 Cu 1.04           ppm Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 29 Cu 20.7           ppm Elemental abundance of the Stannern meteorite sample 1. Classified as a eucrite the sample was taken from a region of the meteorite that was stained yellow. This sample turned out to have higher concentrations of 10 trace elements, upwards of two orders of magnitude, than other eucrites. Laul et al. 1972
Stannern Trend Eucrites 31 Ga 1.36           ppm Laul et al. 1972
Stannern Trend Eucrites 31 Ga 1.36           ppm Elemental abundance of the Stannern meteorite sample 1. Classified as a eucrite the sample was taken from a region of the meteorite that was stained yellow. This sample turned out to have higher concentrations of 10 trace elements, upwards of two orders of magnitude, than other eucrites. Laul et al. 1972
Stannern Trend Eucrites 31 Ga 1.44           ppm Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 31 Ga 1.44           ppm Laul et al. 1972
Stannern Trend Eucrites 49 In 1.17           ppb Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 49 In 4.04           ppb Elemental abundance of the Stannern meteorite sample 1. Classified as a eucrite the sample was taken from a region of the meteorite that was stained yellow. This sample turned out to have higher concentrations of 10 trace elements, upwards of two orders of magnitude, than other eucrites. Laul et al. 1972
Stannern Trend Eucrites 77 Ir 0.12           ppb Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 77 Ir 0.12           ppb Laul et al. 1972
Stannern Trend Eucrites 34 Se 287           ppb Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 34 Se 287           ppb Laul et al. 1972
Stannern Trend Eucrites 81 Tl 24           ppb Elemental abundance of the Stannern meteorite sample 1. Classified as a eucrite the sample was taken from a region of the meteorite that was stained yellow. This sample turned out to have higher concentrations of 10 trace elements, upwards of two orders of magnitude, than other eucrites. Laul et al. 1972
Stannern Trend Eucrites 81 Tl 0.58           ppb Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Stannern Trend Eucrites 30 Zn 40           ppm Elemental abundance of the Stannern meteorite sample 1. Classified as a eucrite the sample was taken from a region of the meteorite that was stained yellow. This sample turned out to have higher concentrations of 10 trace elements, upwards of two orders of magnitude, than other eucrites. Laul et al. 1972
Stannern Trend Eucrites 30 Zn 1.2           ppm Elemental abundance of the Stannern meteorite sample 2. Classified as a eucrite the sample was taken from a region of the meteorite that has a pure white/grey color. Conversley to sample 1, this sample has lower abundances of trace elements. Laul et al. 1972
Washougal Howardite 47 Ag 3.8           ppb Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 79 Au 2.04           ppb Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 83 Bi 0.59           ppb Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 35 Br 59           ppb Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 48 Cd 15           ppb Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 27 Co 43           ppm Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 55 Cs 4.8           ppb Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 29 Cu 3.67           ppm Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 31 Ga 0.96           ppm Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 49 In 13.8           ppb Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 77 Ir 17           ppb Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 34 Se 603           ppb Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 81 Tl 1.8           ppb Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Washougal Howardite 30 Zn 0.9           ppm Elemental abundance of the Washougal meteorite. Classified as a Howardite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Zagami Shergottite 47 Ag 37           ppb Elemental abundance of the Zagami meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Zagami Shergottite 79 Au 2.1           ppb Elemental abundance of the Zagami meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Zagami Shergottite 83 Bi 1.1           ppb Elemental abundance of the Zagami meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Zagami Shergottite 48 Cd 71           ppb Elemental abundance of the Zagami meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Zagami Shergottite 55 Cs 336           ppb Elemental abundance of the Zagami meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Zagami Shergottite 49 In 22.2           ppb Elemental abundance of the Zagami meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Zagami Shergottite 77 Ir 0.1           ppb Elemental abundance of the Zagami meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Zagami Shergottite 37 Rb 6           ppm Elemental abundance of the Zagami meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Zagami Shergottite 34 Se 330           ppb Elemental abundance of the Zagami meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Zagami Shergottite 81 Tl 11           ppb Elemental abundance of the Zagami meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
Zagami Shergottite 30 Zn 55           ppm Elemental abundance of the Zagami meteorite. Classified as a Shergottite, the sample itself consists of material from one or several chips between 500 and 300 mg. No cleaning was attempted prior to irradiation. Laul et al. 1972
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