tab delimited contribution id version timestamp contributor data_model_version reference description 15807 2 2006-12-21T10:05:59.000Z @magic 3.0 10.1016/0012-821X(93)90065-H 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 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 dir_n_samples 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 Deformation Zone Rocks Outcrop 7146 i DE-DI : LT-AF-Z : LT-T-Z:LP-DC4 This study Metamorphic Lamprophyre:altered diorite Superior Province Deformation zone rocks 51.1 51.1 266.1 266.1 North America Canada Ontario 2570 2635 Ma 0 180 -57 3 23 6 20 ND ND ND ND 77 86 3 4 RLG Remanence 100 Related to gold mineralization. RLG Remanence. AF to 100mT, thermal to 580C, characteristic component. IRM (sat. 0. 1T) ; Q. Mean of 3 units calculated. M Red Lake Greenstone Belt Batholiths Outcrop 7145 i DE-DI : LT-AF-Z : LT-T-Z:LP-DC4 This study Intrusive Granite Superior Province Red Lake Greenstone Belt Batholiths 51.1 51.1 266.1 266.1 North America Canada Ontario 2700 2730 Ma 0 159 -74 16 20 14 39 ND ND ND ND 75 222 26 29 RLR Remanence 100 Hammell Lake, Killala Baird, Little Vermilion, Trout Lake. RLR Remanence. AF to 100mT, thermal to 580C, characteristic component. OP (MAGN) ; IRM (sat. 0. 1T) ; Q. Mean of 4 batholiths calculated. M >>>>>>>>>> tab delimited ages location age_low age_high age_unit timescale_eon timescale_era description method_codes timescale_citations citations Deformation Zone Rocks 2570 2635 Ma Archean Neoarchean 40Ar/39Ar ages 2570-2635 at tail of cooling curve. GM-ARAR Gradstein et al. 2004 This study Red Lake Greenstone Belt Batholiths 2700 2730 Ma Archean Neoarchean U-Pb ages 2700-2730 Ma. GM-UPB Gradstein et al. 2004 This study