Primary Data on U/Pb-Isotope Ages and Lu/Hf-Isotope Geochemical Systematization of Detrital Zircons from the Lopatinskii Formation (Vendian–Cambrian Transition Levels) and the Tectonic Nature of Teya–Chapa Depression (Northeastern Yenisei Ridge)


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Аннотация

The main results are presented on U/Pb-isotope dating of 100 detrital zircons and, selectively, on the Lu/Hf-isotope system of 43 grains from sandstones of the Lopatinskii formation (the lower stratigraphic level of the Chingasan group). Ages from 896 ± 51 to 2925 ± 38 Ma were obtained with a pronounced maximum of ~1890 Ma in the curve of probability density, along with εHf estimates from +8.4 to–15.1, which allow one to throw doubt upon the molasse nature of the Lopatinskii formation.

Авторлар туралы

N. Kuznetsov

Geological Institute; Gubkin Russian State University of Oil and Gas

Хат алмасуға жауапты Автор.
Email: kouznikbor@mail.ru
Ресей, Moscow, 119017; Moscow, 119991

N. Priyatkina

Newcastle University

Email: kouznikbor@mail.ru
Австралия, Newcastle-upon-Tyne

S. Rud’ko

Geological Institute

Email: kouznikbor@mail.ru
Ресей, Moscow, 119017

A. Shatsillo

Schmidt Institute of Physics of the Earth

Email: kouznikbor@mail.ru
Ресей, Moscow, 123810

W. Collins

Newcastle University

Email: kouznikbor@mail.ru
Австралия, Newcastle-upon-Tyne

T. Romanyuk

Gubkin Russian State University of Oil and Gas; Schmidt Institute of Physics of the Earth

Email: kouznikbor@mail.ru
Ресей, Moscow, 119991; Moscow, 123810

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