tab delimited	contribution
id	version	timestamp	contributor	data_model_version	reference	description
13526	2	2006-12-22T02:16:58.000Z	@magic	3.0	10.2113/gsecongeo.97.5.997	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	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
Navan Dyke, Baked Contact	Outcrop	8913	i	 DE-DI : LT-AF-Z : LT-T-Z:LP-DC4 	This study	 Metamorphic:Intrusive 	 Dolerite:metamorphics 	East Avalon	Navan Dyke and Baked Contact	53.6	53.6	353.3	353.3	Europe	Ireland	Navan	46	64	Ma	0	182.9	-53.8	4	610	2	ND	ND	C+	ND	70.6	166.1	3.9	5.6		100	Paleocene - Eocene. dip at 10 to 70W. AF and thermal, characteristic component >300C, >80 mT. Secular variations are not avereged.	ND
Navan Zn-Pb Deposit	Outcrop	8912	i	 DE-DI : LT-AF-Z : LT-T-Z:LP-DC4 	This study	 Sedimentary:Metamorphic 	 metamorphics:sediments 	East Avalon	Navan Zn-Pb Deposit	53.6	53.6	353.3	353.3	Europe	Ireland	Navan	318	345	Ma	0	196	6	2.6	147	21	F-	G-	ND	ND	31.8	154.4	1.3	2.6	Overprint	100	Visean - Serpukhovian. Visean - Serpukhovian mineralisation. Overprint. AF and thermal, characteristic component >450C, >120 mT. IRM (PYRR, 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	timescale_stage	description	method_codes	timescale_citations	citations
Navan Dyke, Baked Contact	46	64	Ma	Phanerozoic	Cenozoic	Paleogene	Paleocene : Eocene		K-Ar: 48+/-2, 62+/-2 Ma.	GM-KAR	Gradstein et al. 2004	This study
Navan Zn-Pb Deposit	318	345	Ma	Phanerozoic	Paleozoic	Carboniferous	Mississippian	Visean - Serpukhovian	K-Ar: 366+/-11, 306, 303, 274 Ma.	GM-PMAG-APWP	Gradstein et al. 2004	This study