The Oldest Granites of Russia: Paleoarchean (3343 Ma) Subalkali Granites of the Okhotsk Massif


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Abstract

The Paleoarchean age (3.34 Ga) of subalkali granite magmatism first established for the Kukhtui uplift of the Okhotsk Massif suggests a formation time of the mature continental K-rich crust in this region as early as the Paleoarchean. According to the geological structural, mineralogical–geochemical, geochronological, and isotopic–geochemical data, the Kukhtui uplift can be considered as the most ancient Paleoarchean province in Russia: the ancient consolidation core of the sialic protocrust of the Okhotsk–Omolon Craton.

About the authors

V. K. Kuzmin

Karpinsky All-Russia Geological Research Institute

Author for correspondence.
Email: vkkuzmin@mail.ru
Russian Federation, St. Petersburg, 119106

E. S. Bogomolov

Karpinsky All-Russia Geological Research Institute; Institute of Precambrian Geology and Geochronology

Email: vkkuzmin@mail.ru
Russian Federation, St. Petersburg, 119106; St. Petersburg, 199034

V. A. Glebovitskii

Institute of Precambrian Geology and Geochronology; St. Petersburg State University

Email: vkkuzmin@mail.ru
Russian Federation, St. Petersburg, 199034; St. Petersburg, 199034

N. V. Rodionov

Karpinsky All-Russia Geological Research Institute

Email: vkkuzmin@mail.ru
Russian Federation, St. Petersburg, 119106

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