tab delimited	contribution
id	version	timestamp	contributor	data_model_version	reference	description
14272	2	2006-12-20T11:09:19.000Z	@magic	3.0	10.1139/e91-174	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_comp_name	pole_reversed_perc	description	rock_magnetic_test
Wathaman Batholith, Comp.A	Outcrop	6448	i	 DE-DI : LT-AF-Z : LT-T-Z:LP-DC4 	This study	Intrusive	 mafic dykes:Granite 	Wathaman Batholith	57	57	256.2	256.2	North America	Canada	Saskatchewan	1843	1865	Ma	0	134.6	54.1	3.5	93.6	19	156	ND	ND	IC+	ND	9.3	292.6	3.4	4.9	A	0	A Component. AF to 120mT and thermal to 680C used. IRM (sat. 0. 3T). Inverse Contact Test Parameters: Intruding mafic dyke has positive contact test. Inverse Contact Test Significance: YES.	M
Wathaman Batholith, Comp.B	Outcrop	6449	i	 DE-DI : LT-AF-Z : LT-T-Z:LP-DC4 	This study	Intrusive	 mafic dykes:Granite 	Wathaman Batholith	57	57	256.2	256.2	North America	Canada	Saskatchewan	1800	1850	Ma	0	322.7	-33.9	23.1	29.6	3	12	ND	ND	C+	ND	-8.3	291.7	15.1	26.4	B	100	B Component. AF to 120mT and thermal to 680C used. IRM (sat. 0. 3T). B Component suggested to be about 25Ma younger than A comp. . Contact Test Parameters: Positive contact test with granite. Contact Test Significance: YES.	M
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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
Wathaman Batholith, Comp.A	1843	1865	Ma	Proterozoic	Paleoproterozoic	Orosirian	U-Pb mean age 1854+/-11 Ma.	GM-UPB	Gradstein et al. 2004	This study
Wathaman Batholith, Comp.B	1843	1865	Ma	Proterozoic	Paleoproterozoic	Orosirian	U-Pb mean age 1854+/-11 Ma.	GM-UPB	Gradstein et al. 2004	This study