The Carboniferous of the Moscow syneclise: Paleomagnetic data


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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.

作者简介

A. Iosifidi

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

编辑信件的主要联系方式.
Email: iosag@mail.ru
俄罗斯联邦, St. Petersburg, 191014; St. Petersburg, 191023

V. Mikhailova

All-Russia Petroleum Research Exploration Institute (VNIGRI)

Email: iosag@mail.ru
俄罗斯联邦, St. Petersburg, 191014

V. Popov

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

Email: iosag@mail.ru
俄罗斯联邦, St. Petersburg, 191014; St. Petersburg, 199034

E. Sergienko

St. Petersburg State University

Email: iosag@mail.ru
俄罗斯联邦, St. Petersburg, 199034

A. Danilova

All-Russia Petroleum Research Exploration Institute (VNIGRI)

Email: iosag@mail.ru
俄罗斯联邦, St. Petersburg, 191014

N. Otmas

All-Russia Petroleum Research Exploration Institute (VNIGRI)

Email: iosag@mail.ru
俄罗斯联邦, St. Petersburg, 191014

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