tab delimited	contribution
id	version	timestamp	contributor	data_model_version	reference	description
13870	2	2007-01-19T07:58:26.000Z	@magic	3.0	10.1111/j.1365-246X.1984.tb02874.x	Upgraded to MagIC Data Model 3.0 by the MagIC Database Team
>>>>>>>>>>
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
Batch Volcanics	Outcrop	122	i	 DE-DI : LT-AF-Z:LP-DC3 	This study	Extrusive	Extrusives	Batch volcanics	52.5	52.5	357.2	357.2	Europe	U.K.	U.K.	530	540	Ma	100	321.8	14.5	21.8	10.4	6	33	ND	ND	IC+	ND	35	226	11	22.6	0	Post Uriconian represented by tuff bands in Synalds Group. . Uniform dip to NW. . AF best, thermal causes chemical changes in tuffs. . Js-T (CT 590-680C). In situ close to present field, but see FIELDTESTS. Inverse Contact Test Parameters: One tuff remagnetised by early Palaeozoic dykes. . Inverse Contact Test Significance: YES.	M
Batch Volcanics	Outcrop	122	i	 DE-DI : LT-AF-Z:LP-DC3 	This study	Extrusive	Extrusives	Batch volcanics	52.5	52.5	357.2	357.2	Europe	U.K.	U.K.	530	540	Ma	0	16.3	68.5		10	6		ND	ND	IC+	ND	35	226	11	22.6	0	Post Uriconian represented by tuff bands in Synalds Group. . Uniform dip to NW. . AF best, thermal causes chemical changes in tuffs. . Js-T (CT 590-680C). In situ close to present field, but see FIELDTESTS. Inverse Contact Test Parameters: One tuff remagnetised by early Palaeozoic dykes. . Inverse Contact Test Significance: YES.	M
Longmyndian Sediments	Outcrop	121	i	 DE-DI : LT-AF-Z : LT-CHEM : LT-T-Z:LP-DC3 	This study	Sedimentary	sediments	Longmyndian sediments	52.6	52.6	357.2	357.2	Europe	U.K.	Wales	530	540	Ma	0	116	76.2	6.2	20.3	28	166	ND	ND	ND	ND	36.4	26.8	10.6	11.4	-1	Overlie Uriconian Grp-558, & post Uriconian granophyre-533Ma. . AF (140mT) , Th (660C) , Chem (1000hrs). Th. best. Sing. comp. only used. Js-T (CT 620-680C, inflexion point in range 550-590C). . Fold test cannot be applied, non-Fisherian. In situ better grp.	M
>>>>>>>>>>
tab delimited	ages
location	age_low	age_high	age_unit	timescale_eon	timescale_era	timescale_period	timescale_epoch	description	method_codes	timescale_citations	citations
Batch Volcanics	530	540	Ma	Phanerozoic	Paleozoic	Cambrian	Early Cambrian	Rb-Sr on late or post-Uriconian granophyre 533+/-13.	GM-RBSR	Gradstein et al. 2004	This study
Longmyndian Sediments	530	540	Ma	Phanerozoic	Paleozoic	Cambrian	Early Cambrian	Rb-Sr is. 516+/-6, 448+/-31; Fission track 526+/-8, 528+/-41Ma.	 GM-RBSR:GM-FT 	Gradstein et al. 2004	This study