tab delimited contribution id version timestamp contributor data_model_version reference description 13516 2 2006-12-21T09:55:33.000Z @magic 3.0 10.1016/0031-9201(73)90012-5 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 Elmina Sandstone Outcrop 2750 i DE-DI : LT-NO:LP-DC1 This study Sedimentary purplesandstone Elmina Sandstone 5 5 358.2 358.2 Africa Ghana Ghana 100 146 Ma 100 334 11.5 12.1 13.8 12 25 ND ND ND ND 64 271 6.2 12.3 0 Sekondi Series. Superseded study. Thermal to 600C causes general increase in dispersion. Early to mid Cretaceous remagnetization suggested. Old Result. Superseded study. ND Elmina Sandstone Outcrop 2750 i DE-DI : LT-NO:LP-DC1 This study Sedimentary purplesandstone Elmina Sandstone 5 5 358.2 358.2 Africa Ghana Ghana 100 146 Ma 0 330 38.5 13.6 11.2 12 ND ND ND ND 64 271 6.2 12.3 0 Sekondi Series. Superseded study. Thermal to 600C causes general increase in dispersion. Early to mid Cretaceous remagnetization suggested. Old Result. Superseded study. ND Elmina Sandstone Outcrop 2750 i DE-DI : LT-NO:LP-DC1 This study Sedimentary purplesandstone Elmina Sandstone 5 5 358.2 358.2 Africa Ghana Ghana 100 146 Ma 0 334 11.5 12.1 13.8 12 ND ND ND ND 64 271 6.2 12.3 0 Sekondi Series. Superseded study. Thermal to 600C causes general increase in dispersion. Early to mid Cretaceous remagnetization suggested. Old Result. Superseded study. ND >>>>>>>>>> tab delimited ages location age_low age_high age_unit timescale_eon timescale_era timescale_period method_codes timescale_citations citations Elmina Sandstone 359 416 Ma Phanerozoic Paleozoic Devonian GM-CC-STRAT Gradstein et al. 2004 This study