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Russian Journal of Pacific Geology

, Volume 12, Issue 4, pp 320–339 | Cite as

Sedimentation Conditions and Provenance Composition of the Upper Jurassic–Lower Cretaceous Deposits of the Upper Pegtymel Depression, Chukotka Terrane

  • E. V. Vatrushkina
  • M. I. Tuchkova
Article
  • 12 Downloads

Abstract

The deposits of the Imlekin Formation of the Upper Pegtymel depression were formed in the southern margin of the Chukotka Terrane synchronously with accretion of the Kulpolney island arc to the Chukotka–Arctic Alaska microplate. The sedimentological structural features of the Upper Jurassic–Lower Cretaceous sections indicate their accumulation within various parts of submarine fans of a shallow marine basin. The submarine slump origin of the boulder–pebble (tillite-like) conglomerates is substantiated. The petrographic, geochemical, and geochronological methods identified two dominant provenances: Triassic clastic rocks and Volgian suprasubduction volcanic rocks. The Middle Volgian–Early Berriasian age of the Imlekin Formation is specified. The geodynamic model proposed explains the change of the sources and direction of the sediment transport in the Volgian.

Keywords:

volcanoclastic complexes turbidites tilloids arc–continent collision zircon dating Chukotka Terrane northeast Russia 

Notes

ACKNOWLEDGMENTS

The authors are grateful to the reviewers for constructive criticism and recommendations. This work was supported by the Russian Science Foundation (project no 16-17-10251). The staff of the Geological Institute, Russian Academy of Sciences was supported by the Federal Agency on Science Organizations (project no. 0135-2016-0022 “Geodynamic Aspects of Structure-Forming, Magmatic, and Sedimentary Processes of the Paleozoic–Mesozoic Evolution of the Northwestern Sector of Pacific Belt”).

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Copyright information

© Pleiades Publishing, Ltd. 2018

Authors and Affiliations

  1. 1.Geological Institute, Russian Academy of SciencesMoscowRussia

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