tab delimited	contribution
id	version	timestamp	contributor	data_model_version	reference	description
12277	2	2006-12-19T07:36:37.000Z	@magic	3.0	10.1016/0012-821X(86)90197-4	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
Elatina Formation, Adelaide Geosyncline	Outcrop	560	i	 DE-VGP : LT-T-Z:LP-DC4 	This study	Sedimentary	 Sandstone:Redbeds 	Elatina Formation	-32.4	-32.4	138	138	Australia	Australia	South Australia	590	610	Ma	100	191.9	-9.6	3.4	384.6	6	37	ND	ND	ND	ND	50.9	157.1	2.2	2.2	0	Marinoan glaciation - See REFNOS 48, 982 for suggested ages. Strikes 148-173/Dips 14-33. Fold axis plunge 93-123/13-14S. . Thermal to 680C. PCA in range 650-680C. . OP (HEM in intersticial clays+minor GOETH, MART) , SUSC, AN. See RESULTNO 6354 for evidence of magnetisation age.	M
Elatina Formation, Adelaide Geosyncline	Outcrop	560	i	 DE-VGP : LT-T-Z:LP-DC4 	This study	Sedimentary	 Sandstone:Redbeds 	Elatina Formation	-32.4	-32.4	138	138	Australia	Australia	South Australia	590	610	Ma	0	194.1	2.4	3.5	357.1	6		ND	ND	ND	ND	50.9	157.1	2.2	2.2	0	Marinoan glaciation - See REFNOS 48, 982 for suggested ages. Strikes 148-173/Dips 14-33. Fold axis plunge 93-123/13-14S. . Thermal to 680C. PCA in range 650-680C. . OP (HEM in intersticial clays+minor GOETH, MART) , SUSC, AN. See RESULTNO 6354 for evidence of magnetisation age.	M
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tab delimited	ages
location	age_low	age_high	age_unit	timescale_eon	timescale_era	timescale_period	method_codes	timescale_citations	citations
Elatina Formation, Adelaide Geosyncline	590	610	Ma	Proterozoic	Neoproterozoic	Cryogenian : Ediacaran	GM-CC-STRAT	Gradstein et al. 2004	This study