tab delimited contribution id version timestamp contributor data_model_version reference description 15102 2 2006-12-22T01:52:41.000Z @magic 3.0 10.1016/S0012-821X(00)00026-1 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 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 Bulla, Siusi Sections in Dolomites Outcrop 8674 i DE-DI : LT-AF-Z : LT-T-Z:LP-DC4 This study Sedimentary Sandstone:Limestone 46.5 46.5 11.6 11.6 Europe Italy Southern Alps 248 254 Ma 100 335.3 17.1 6.8 999.9 2 322 F+ ND ND R- 46.7 228.6 3.6 7 51 Permian-Triassic boundary. Extent 20 km. AF and thermal, characteristic component. IRM (MAGN, GOETH) , SUSC. ND Bulla, Siusi Sections in Dolomites Outcrop 8674 i DE-DI : LT-AF-Z : LT-T-Z:LP-DC4 This study Sedimentary Sandstone:Limestone 46.5 46.5 11.6 11.6 Europe Italy Southern Alps 248 254 Ma 100 335.3 17.1 6.8 999.9 322 F+ ND ND R- 46.7 228.6 3.6 7 51 Permian-Triassic boundary. Extent 20 km. AF and thermal, characteristic component. IRM (MAGN, GOETH) , SUSC. ND Bulla, Siusi Sections in Dolomites Outcrop 8674 i DE-DI : LT-AF-Z : LT-T-Z:LP-DC4 This study Sedimentary Sandstone:Limestone 46.5 46.5 11.6 11.6 Europe Italy Southern Alps 248 254 Ma 0 335.1 6.8 53.9 23.7 322 F+ ND ND R- 46.7 228.6 3.6 7 51 Permian-Triassic boundary. Extent 20 km. AF and thermal, characteristic component. IRM (MAGN, GOETH) , SUSC. ND >>>>>>>>>> tab delimited ages location age_low age_high age_unit timescale_eon timescale_era timescale_period timescale_epoch method_codes timescale_citations citations Bulla, Siusi Sections in Dolomites 248 254 Ma Phanerozoic Paleozoic : Mesozoic Permian : Triassic Lopingian : Early Triassic GM-FOSSIL Gradstein et al. 2004 This study