tab delimited	contribution
id	version	timestamp	contributor	data_model_version	reference	description
15904	2	2007-01-18T10:15:38.000Z	@magic	3.0	10.1016/0012-821X(77)90009-7	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_n_sites	dir_n_samples	fold_test	conglomerate_test	contact_test	reversal_test	pole_lat	pole_lon	pole_dp	pole_dm	pole_reversed_perc	description	rock_magnetic_test
Giant Gabbro Dykes, Tugtutoq Island	Outcrop	2131	i	 DE-DI : LT-AF-Z:LP-DC3 	This study	Intrusive	Gabbro		60.9	60.9	313.7	313.7	Greenland	Denmark	Greenland	1118	1192	Ma	0	292.2	56.5	7.6	30	13	73	ND	ND	ND	ND	42.3	226.1	8	11.1	0	AF cleaning 15-30mT. Js-T (CT 475-530C).	M
Hriddal Giant Dyke	Outcrop	2132	i	 DE-DI : LT-AF-Z:LP-DC3 	This study	Intrusive	syenite dyke	Hriddal Giant Dyke	60.9	60.9	313.7	313.7	Greenland	Denmark	Greenland	1153	1171	Ma	0	294.3	42.7	9.8	38	7	38	ND	ND	ND	ND	33.2	215.3	7.6	12.2	0	AF cleaning 15-30mT.	ND
Narssaq Gabbro	Outcrop	2133	i	 DE-DI : LT-AF-Z:LP-DC3 	This study	Intrusive	Gabbro	Narssaq Gabbro	60.9	60.9	313.8	313.8	Greenland	Denmark	Greenland	1153	1171	Ma	0	285.3	46.8	9.4	97	4	22	ND	ND	ND	ND	31.6	225.4	7.8	12.1	0	Mainland equivalent of Hriddal Giant Dyke. AF cleaning 15-30mT.	ND
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tab delimited	ages
location	age_low	age_high	age_unit	timescale_eon	timescale_era	timescale_period	description	method_codes	timescale_citations	citations
Giant Gabbro Dykes, Tugtutoq Island	1118	1192	Ma	Proterozoic	Mesoproterozoic	Stenian	Rb-Sr isochron 1155+/-37 Ma.	GM-RBSR	Gradstein et al. 2004	This study
Hriddal Giant Dyke	1153	1171	Ma	Proterozoic	Mesoproterozoic	Stenian	Rb-Sr isochron 1162+/-9 Ma.	GM-RBSR	Gradstein et al. 2004	This study
Narssaq Gabbro	1153	1171	Ma	Proterozoic	Mesoproterozoic	Stenian	Rb-Sr age 1162+/-9 Ma.	GM-RBSR	Gradstein et al. 2004	This study