tab delimited	contribution
id	version	timestamp	contributor	data_model_version	reference	description
14410	2	2006-12-21T11:55:53.000Z	@magic	3.0	10.1029/95TC03499	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	terranes	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_significance	fold_test	conglomerate_test	contact_test	reversal_test	pole_lat	pole_lon	pole_dp	pole_dm	pole_reversed_perc	description	rock_magnetic_test
Intermontane Belt Plutonic Rocks	Outcrop	8035	i	 DE-VGP : LT-AF-Z : LT-T-Z:LP-DC4 	This study	Intrusive	 quartzdiorite:Granodiorite 	Terrane I	Intermontane Belt Plutonic Rocks	56.6	56.6	233.8	233.8	North America	Canada	British Columbia	65	83	Ma	100	158	-69	4	999.9	3	35	95	F+	ND	ND	Ro	76.6	134	6.3	6.3	67	Located in Finaly-Ingenika Fault Zone. AF to 100mT, thermal to 700C, characteristic component. IRM. Magnetization probably acquired after KN Superchron. Corrections for block rotations improve grouping.	M
Intermontane Belt Plutonic Rocks	Outcrop	8035	i	 DE-VGP : LT-AF-Z : LT-T-Z:LP-DC4 	This study	Intrusive	 quartzdiorite:Granodiorite 	Terrane I	Intermontane Belt Plutonic Rocks	56.6	56.6	233.8	233.8	North America	Canada	British Columbia	65	83	Ma	0	194	-70	11	139	3		95	F+	ND	ND	Ro	76.6	134	6.3	6.3	67	Located in Finaly-Ingenika Fault Zone. AF to 100mT, thermal to 700C, characteristic component. IRM. Magnetization probably acquired after KN Superchron. Corrections for block rotations improve grouping.	M
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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
Intermontane Belt Plutonic Rocks	120	175	Ma	Phanerozoic	Mesozoic	Jurassic : Cretaceous	Middle Jurassic : Early Cretaceous	K-Ar ages 122+/-6 to 174+/-5 Ma.	GM-KAR	Gradstein et al. 2004	This study