Detrital zircon ages from upper Paleozoic–Triassic clastic strata on St. Lawrence Island, Alaska: An enigmatic component of the Arctic Alaska–Chukotka microplate

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چکیده

Abstract New lithologic and detrital zircon (DZ) U-Pb data from Devonian–Triassic strata on St. Lawrence Island in the Bering Sea western Brooks Range of Alaska suggest affinities between these two areas. The constitutes part Arctic Alaska–Chukotka microplate, but tectonic paleogeographic are unknown or at best speculative. Strata form a carbonate succession Mississippian(?)–Triassic clastic that subdivided according to three distinctive DZ age distributions. has Mississippian-age quartz arenite beds with Silurian, Cambrian, Neoproterozoic, Mesoproterozoic modes, it exhibits similar distributions biostratigraphic characteristics as Utukok Formation Kelly River allochthon Range. Consistent late Silurian ages each units efficient mixing prior deposition, derivation exposed by pre-Mississippian unconformity and/or Endicott Group postdate unconformity. is into feldspathic graywacke subunits. subunit unimodal mode 2.06 Ga, identical Nuka Ridge Range, records depositional episode related Paleozoic juxtaposition Paleoproterozoic terrane along most distal parts microplate. Triassic maximum abundant grains, likely sourced fringing arcs continent-scale paleorivers draining Eurasia, Lisburne Peninsula (northwestern Alaska), Chukotka Wrangel (eastern Russia), northern Sverdrup Basin (Canadian Arctic), but, unlike succession, no obvious analogue stack. These correlations establish conclusively belonging thus enhancing our understanding circum-Arctic region Paleozoic–Triassic time.

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ژورنال

عنوان ژورنال: Geosphere

سال: 2022

ISSN: ['1553-040X']

DOI: https://doi.org/10.1130/ges02490.1