tab delimited contribution id version timestamp contributor data_model_version reference description 13998 2 2006-12-19T12:09:18.000Z @magic 3.0 10.1098/rsta.1957.0013 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_k_ratio dir_n_sites dir_n_samples fold_test_significance fold_test conglomerate_test contact_test reversal_test pole_lat pole_lon pole_dp pole_dm pole_reversed_perc description rock_magnetic_test Lower Torridonian Sandstone Outcrop 3766 i DE-DI : LT-NO:LP-DC0 This study Sedimentary Redbeds Torridonian Sandstone 58 58 354 354 Europe U.K. Scotland 755 803 Ma 100 307 34 7 40 5.79 13 32 99 F+ G+ ND ND 35 242 5 8 0 Daibaig Group. Superseded study. Old Result. Superseded study. Conglomerate Test Parameters: Conglomerate pebbles scattered. Conglomerate Test Significance: YES. ND Upper Torridonian Sandstone Outcrop 3765 i DE-DI : LT-NO:LP-DC1 This study Sedimentary sediments Torridonian Sandstone 58 58 354 354 Europe U.K. Scotland 755 803 Ma 100 123 44 5 12 5.79 81 205 99 F+ G+ ND Ro 6 43 4 6 35 Applecross and Aultbea Groups. Extent Thickness 3000m. Superseded study. Thermal demagnetization tests carried out. Old Result. Superseded study. Conglomerate Test Parameters: Conglomerate pebbles have scattered directions. Conglomerate Test Significance: YES. ND >>>>>>>>>> tab delimited ages location age_low age_high age_unit timescale_eon timescale_era timescale_period description method_codes timescale_citations citations Lower Torridonian Sandstone 755 803 Ma Proterozoic Neoproterozoic Cryogenian Rb-Sr age 779+/-24 Ma - see REFNO 263. GM-RBSR Gradstein et al. 2004 This study Upper Torridonian Sandstone 755 803 Ma Proterozoic Neoproterozoic Cryogenian Rb-Sr age 779+/-24 Ma - see REFNO 263. GM-RBSR Gradstein et al. 2004 This study