tab delimited	contribution
id	version	timestamp	contributor	data_model_version	reference	description
14417	3	2006-12-22T12:33:40.000Z	@magic	3.0	10.1016/S0040-1951(97)00065-6	Upgraded to MagIC Data Model 3.0 by the MagIC Database Team
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tab delimited	locations
location	location_type	result_name	result_type	method_codes	citations	geologic_classes	lithologies	geological_province_sections	lat_s	lat_n	lon_w	lon_e	continent_ocean	country	region	age_low	age_high	age_unit	dir_tilt_correction	dir_dec	dir_inc	dir_alpha95	dir_k	dir_k_ratio	dir_n_sites	dir_n_samples	fold_test_significance	fold_test	conglomerate_test	contact_test	reversal_test	pole_lat	pole_lon	pole_dp	pole_dm	pole_comp_name	pole_reversed_perc	description	rock_magnetic_test
Harachiyama Formation, High-T	Outcrop	8216	i	 DE-DI : LT-T-Z:LP-DC4 	This study	Extrusive	welded tuff	Harachiyama Formation	39.5	39.5	142	142	Asia	Japan	Omoe Peninsula	114	119	Ma	100	94.2	20.4	43.7	34.8		2	22		ND	ND	ND	ND	-3.5	41.2	24	45.8	High-T	100	High Temp. . Thermal to 680C, high temp. component >560C. IRM (no sat. 2. 7T).	M
Harachiyama Formation, High-T	Outcrop	8216	i	 DE-DI : LT-T-Z:LP-DC4 	This study	Extrusive	welded tuff	Harachiyama Formation	39.5	39.5	142	142	Asia	Japan	Omoe Peninsula	114	119	Ma	0	90.4	-4.7	72.1	14.2		2			ND	ND	ND	ND	-3.5	41.2	24	45.8	High-T	100	High Temp. . Thermal to 680C, high temp. component >560C. IRM (no sat. 2. 7T).	M
Harachiyama Formation, Med-T	Outcrop	8217	i	 DE-DI : LT-T-Z:LP-DC4 	This study	Extrusive	welded tuff	Harachiyama Formation	39.5	39.5	142	142	Asia	Japan	Omoe Peninsula	114	119	Ma	100	281	17.3	26.7	89.8		2	22		ND	ND	ND	ND	14.1	51.9	14.3	27.6	Medium Temp.	0	Medium Temp. . Thermal to 680C, medium temp. component <560C. IRM (no sat. 2. 7T).	M
Harachiyama Formation, Med-T	Outcrop	8217	i	 DE-DI : LT-T-Z:LP-DC4 	This study	Extrusive	welded tuff	Harachiyama Formation	39.5	39.5	142	142	Asia	Japan	Omoe Peninsula	114	119	Ma	0	283.4	-14.3	72.7	14		2			ND	ND	ND	ND	14.1	51.9	14.3	27.6	Medium Temp.	0	Medium Temp. . Thermal to 680C, medium temp. component <560C. IRM (no sat. 2. 7T).	M
Harachiyama Formation, Med-T	Outcrop	8217	i	 DE-DI : LT-T-Z:LP-DC4 	This study	Extrusive	welded tuff	Harachiyama Formation	39.5	39.5	142	142	Asia	Japan	Omoe Peninsula	114	119	Ma	0	281	17.3	26.7	89.8		2			ND	ND	ND	ND	14.1	51.9	14.3	27.6	Medium Temp.	0	Medium Temp. . Thermal to 680C, medium temp. component <560C. IRM (no sat. 2. 7T).	M
Heizaki Volcanics	Outcrop	8215	i	 DE-VGP : LT-AF-Z : LT-T-Z:LP-DC4 	This study	Extrusive	welded tuff	Heizaki Volcanics	39.6	39.6	142	142	Asia	Japan	Omoe Peninsula	62	71	Ma	100	283.5	9.4	8	58	0.44	7	83	10	Fo	ND	ND	ND	13.4	47.4	4.7	4.7		0	Thermal to 650C, characteristic component. IRM (sat. 0. 3T).	M
Heizaki Volcanics	Outcrop	8215	i	 DE-VGP : LT-AF-Z : LT-T-Z:LP-DC4 	This study	Extrusive	welded tuff	Heizaki Volcanics	39.6	39.6	142	142	Asia	Japan	Omoe Peninsula	62	71	Ma	0	284.7	-17	5.3	131.1		7		10	Fo	ND	ND	ND	13.4	47.4	4.7	4.7		0	Thermal to 650C, characteristic component. IRM (sat. 0. 3T).	M
Miyako-Oura Granire	Outcrop	8218	i	 DE-DI : LT-T-Z:LP-DC4 	This study	Intrusive	Granite	Miyako-Oura Granire	39.5	39.5	142	142	Asia	Japan	Omoe Peninsula	109	135	Ma	0	298.9	46.8	58.3	20.5		2	24		ND	ND	ND	ND	38.9	58.7	48.5	75.2		0	Thermal to 620C, characteristic component >450C.	ND
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tab delimited	ages
location	age_low	age_high	age_unit	timescale_eon	timescale_era	timescale_period	timescale_epoch	description	method_codes	timescale_citations	citations
Harachiyama Formation, High-T	114	119	Ma	Phanerozoic	Mesozoic	Cretaceous	Early Cretaceous	Isotopic ages 144-119 Ma cited.	GM-ISO	Gradstein et al. 2004	This study
Harachiyama Formation, Med-T	114	119	Ma	Phanerozoic	Mesozoic	Cretaceous	Early Cretaceous	Isotopic ages 144-119 Ma cited.	GM-ISO	Gradstein et al. 2004	This study
Heizaki Volcanics	62	71	Ma	Phanerozoic	Mesozoic : Cenozoic	Cretaceous : Paleogene	Late Cretaceous : Paleocene	K-Ar age 62. 2+/-2. 5 Ma; 40Ar/39Ar age 71. 3+/-2. 4 Ma.	 GM-KAR:GM-ARAR 	Gradstein et al. 2004	This study
Miyako-Oura Granire	109	135	Ma	Phanerozoic	Mesozoic	Cretaceous	Early Cretaceous	Isotopic ages 109-135 Ma cited.	GM-ISO	Gradstein et al. 2004	This study