tab delimited contribution id version timestamp contributor data_model_version reference description 15568 2 2007-01-18T10:42:17.000Z @magic 3.0 10.1111/j.1365-246X.1979.tb01022.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_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 Amana-Talampaya Formation Outcrop 6 i DE-VGP : LT-CHEM : LT-T-Z:LP-DC3 This study Sedimentary Redbeds Amana-Talampaya Formation -30 -30 293 293 South America Argentina Argentina 245 260 Ma 100 172.4 7.9 14 ND ND ND Ro 63 276 11 11 200 Upper section of Paganzo Group, formerly Paganzo III. . Av. Strike 52/Dip 13 SE. . Optimum temp. 250-300C, optimum chemical 700hrs. . 40 deg. VGP cut off applied. . ND La Colina Formation Outcrop 7 i DE-VGP : LT-AF-Z : LT-CHEM : LT-T-Z:LP-DC3 This study Extrusive:Sedimentary Extrusives La Colina Formation -30 -30 293 293 South America Argentina Argentina 299 318 Ma 100 131.4 65.7 57 ND ND Co ND 49 163 5 5 100 Section II, Paganzo Group (formerly Paganzo II). . Av. Strike 001/Dip 18 E. AF lavas 20mT, Th 250-300C, Chem 700hrs. . 40 deg. VGP cut off applied. . Contact Test Parameters: Lavas and baked seds agree, but unbaked seds ?. Contact Test Significance: ?. ND >>>>>>>>>> tab delimited ages location age_low age_high age_unit timescale_eon timescale_era timescale_period timescale_epoch description method_codes timescale_citations citations Amana-Talampaya Formation 245 260 Ma Phanerozoic Paleozoic : Mesozoic Permian : Triassic Lopingian : Early Triassic GM-CC-STRAT Gradstein et al. 2004 This study La Colina Formation 299 318 Ma Phanerozoic Paleozoic Carboniferous Pennsylvanian K-Ar lavas (295+/-5). GM-ISO:GM-CC-STRAT Gradstein et al. 2004 This study