Cretaceous plutonic rocks of St. Lawrence Island, Alaska; a preliminary report

Bela Csejtey; William Wallace Patton; Thomas P. Miller

doi:10.3133/ofr7182

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Cretaceous plutonic rocks of St. Lawrence Island, Alaska; a preliminary report

Bela Csejtey·William Wallace Patton·Thomas P. Miller

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Abstract

Reconnaissance mapping on St. Lawrence Island, Alaska has revealed seven epizonal granitic plutons of mid-Cretaceous age with a combined outcrop area of about 350 square miles. The plutonic rocks are dominantly quartz monzonite, but include minor amounts of granodiorite, monzonite, syenite, syenodiorite, and alaskite. The plutons are structurally and petrologically similar to and about the same age as plutons on the Chukotsky Peninsula, U.S.S.R. and in western Alaska. They suggest tectonic continuity between Siberia and Alaska since at least Cretaceous time. Several mineralized areas containing molybdenum, copper, lead, and zinc sulfides are associated with the plutonic bodies in the western part of the island.

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Source-reported bounding extent: 62.694309593663185° to 64.06259063688063° latitude; -171.93603515625° to -168.64013671875° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Bela Csejtey, William Wallace Patton, Thomas P. Miller. 1971. Cretaceous plutonic rocks of St. Lawrence Island, Alaska; a preliminary report. https://doi.org/10.3133/ofr7182

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