tab delimited	contribution
id	version	timestamp	contributor	data_model_version	reference	description
13234	2	2006-12-22T02:27:38.000Z	@magic	3.0	10.1046/j.1365-246X.2003.01923.x	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	pole_antipodal_angle	description	rock_magnetic_test
El Quemado Formation	Outcrop	8973	i	 DE-VGP : LT-AF-Z : LT-T-Z:LP-DC4 	This study	Extrusive	 Tuff:ignimbrite 	El Quemado Formation	-47.43	-47.43	288.23	288.23	South America	Argentina	Patagonia	155	159	Ma	100	11.3	-61	5.4	47	16	154	F+	ND	ND	Rb	81	352	8	8	88	174	Upper Jurassic. AF and thermal, characteristic component 400-590C, 50-100 mT. IRM, 3-axis Jrs-T, Hyst, Js-T, OP (MAGN, HEM). Localities north of 49 degrees S only.	ND
Marifil Formation	Outcrop	8972	i	 DE-VGP : LT-AF-Z : LT-T-Z:LP-DC4 	This study	Extrusive	 Dacite: Tuff :ignimbrite 	Marifil Formation	-44.75	-44.75	294.417	294.417	South America	Argentina	Patagonia	166	188	Ma	0	2.9	-57	8.7	32	10	71	ND	ND	ND	Rc	83	318	11.3	11.3	30	175.2	Middle Jurassic. Extent 30 km. AF and thermal, characteristic component 400-590C, 50-100 mT. IRM, 3-axis Jrs-T, Hyst, Js-T, OP (MAGN, HEM).	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
El Quemado Formation	155	159	Ma	Phanerozoic	Mesozoic	Jurassic	Late Jurassic	40Ar/39Ar age 157+/-2 Ma.	 GM-CC-STRAT:GM-ARAR 	Gradstein et al. 2004	This study
Marifil Formation	166	188	Ma	Phanerozoic	Mesozoic	Jurassic	Middle Jurassic	Rb-Sr and 40Ar/39Ar ages between 166 and 188 Ma.	 GM-CC-STRAT : GM-RBSR:GM-ARAR 	Gradstein et al. 2004	This study