데이터셋 상세
캐나다
Preliminary bedrock geology map of the Rusty Mountain and Bonnet Plume Pass areas, southern Wernecke Mountains, Yukon (NTS 106C/3, 4, 5, 6, 11, 12 and 106D/1, 8)
not_specified
데이터 정보
연관 데이터
Preliminary bedrock geology map of the southern Rusty Mountain area, southern Wernecke Mountains, Yukon (parts of NTS 106C/4,5 and 106D/1,8)
공공데이터포털
not_specified
Preliminary bedrock geology of the Mt. Decoeli area (parts of NTS 115A/12, 13 and 115B/9, 16)
공공데이터포털
not_specified
Bedrock Geology, Miles Ridge area, Yukon, (parts of NTS 115F/15, 16 and 115K/1,2)
공공데이터포털
not_specified
Surficial Geology of the Howard’s Pass area (NTS 105I/12 and parts of 105I/11, 6 and 5 and 105J/9 and 8 ), Yukon and Northwest Territories
공공데이터포털
not_specified
Bedrock geology compilation of the eastern Rackla belt, NTS 105N/15, 105N/16, 105O/13, 106B/4, 106C/1, 106C/2, east-central Yukon
공공데이터포털
not_specified
Surficial Geology of the Howard’s Pass Area (NTS 105I/11 and parts of 105I/10, 6 and 7), Yukon and Northwest Territories
공공데이터포털
not_specified
Update on the bedrock geology of the Rusty Mountain area, southern Wernecke Mountains, Yukon (parts of NTS 106C/4, 5, 12 and 106D/1, 8)
공공데이터포털
The Rusty Mountain area is underlain by sedimentary strata of the Paleoproterozoic Wernecke Supergroup, Mesoproterozoic Pinguicula Group, Neoproterozoic Hematite Creek Group and Windermere Supergroup, and Paleozoic Bouvette Formation. Three suites of intrusions are documented: (1) 10–200 m thick, subalkaline, mafic sills and dikes of the ca. 1380 Ma Hart River suite intrude the Wernecke Supergroup; (2) 2–3 m wide, vertical, east-west striking, alkaline, mafic dikes that are geochemically distinct from the Hart River suite intrude the Wernecke Supergroup; and (3) a 30 cm thick, mafic, porphyritic dike intrudes the Wernecke Supergroup at one locality. The main structures in the Wernecke Supergroup are northwest-verging folding and thrusting and a steeply dipping axial-planar cleavage. This deformation affected the Hart River sills, but not the east-west striking dikes. The main structures in the Pinguicula Group and younger strata are northwest-southeast trending gentle folds and a steeply dipping axial-planar cleavage.
Bedrock geology map of the Teslin Mountain and east Lake Laberge areas
공공데이터포털
not_specified
Bedrock geology of the Tay Mountain area, central Yukon
공공데이터포털
not_specified
Bedrock geology map of the Teslin Mountain and East Lake Laberge areas, parts of NTS 105E/2, 3 and 6
공공데이터포털
not_specified
목록