Sr isotopic chemostratigraphy of Precambrian carbonate rocks in the Amderma Rise, Pai-Khoi Ridge


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Аннотация

The Sr and C isotopic compositions of Precambrian carbonate rocks are determined for Amderma Rise, in the northeastern margin of Pai-Khoi Ridge. Based on the Sr isotopic chemostratigraphy, it is established for the first time that the Amderma Formation is referred to the Early Vendian, while the Morozovsk Formation is Late Riphean in age. This conclusion along with detailed mapping proves that the Precambrian “section” of the Amderma Rise is a series of tectonic plates combined in a nonchronostratigraphic order. Volcanic and sedimentary rocks of the Morozovsk and Sokolninsk formations make up the allochthon proper, while carbonate rocks of the Amderma Formation make up the para-autochthon. The high values of δ13С (up to +9.5‰) identified in limestones of both formations suggest a considerable distance of the Pai-Khoi paleobasin from the passive margin of the Baltic Region upon facies similarity to the Laurentia active margins.

Авторлар туралы

A. Kuznetsov

Institute of Precambrian Geology and Geochronology

Хат алмасуға жауапты Автор.
Email: antonbor9@mail.ru
Ресей, nab. Makarova 2, St. Petersburg, 199034

E. Starikova

Institute of Precambrian Geology and Geochronology

Email: antonbor9@mail.ru
Ресей, nab. Makarova 2, St. Petersburg, 199034

A. Maslov

Institute of Geology and Geochemistry, Ural Branch

Email: antonbor9@mail.ru
Ресей, ul. Vonsovskogo 15, Yekaterinburg, 620016

G. Konstantinova

Institute of Precambrian Geology and Geochronology

Email: antonbor9@mail.ru
Ресей, nab. Makarova 2, St. Petersburg, 199034

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