The Carboniferous of the Moscow syneclise: Paleomagnetic data


Дәйексөз келтіру

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Аннотация

New data for the Early and Late Carboniferous sections of the Russian platform (Moscow syneclise and Donbass) are presented. Magneto-mineralogical studies are carried out to identify the magnetic minerals—carriers of natural remanent magnetization. Extensive Late Paleozoic remagnetization of Carboniferous rocks is revealed. The obtained paleomagnetic data allowed us to determine the average paleomagnetic poles for the Gzhelian, Serpukhovian, and Visean stages of Carboniferous deposits of the Moscow syneclise.

Авторлар туралы

A. Iosifidi

All-Russia Petroleum Research Exploration Institute (VNIGRI); Institute of Terrestrial Magnetism, Ionosphere and Radiowave Propagation, St. Petersburg Branch

Хат алмасуға жауапты Автор.
Email: iosag@mail.ru
Ресей, St. Petersburg, 191014; St. Petersburg, 191023

V. Mikhailova

All-Russia Petroleum Research Exploration Institute (VNIGRI)

Email: iosag@mail.ru
Ресей, St. Petersburg, 191014

V. Popov

All-Russia Petroleum Research Exploration Institute (VNIGRI); St. Petersburg State University

Email: iosag@mail.ru
Ресей, St. Petersburg, 191014; St. Petersburg, 199034

E. Sergienko

St. Petersburg State University

Email: iosag@mail.ru
Ресей, St. Petersburg, 199034

A. Danilova

All-Russia Petroleum Research Exploration Institute (VNIGRI)

Email: iosag@mail.ru
Ресей, St. Petersburg, 191014

N. Otmas

All-Russia Petroleum Research Exploration Institute (VNIGRI)

Email: iosag@mail.ru
Ресей, St. Petersburg, 191014

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