Carboniferous of the Russian Platform: Paleomagnetic Data

被引：2

作者：

Iosifidi, A. G. ^{[1
,4
]}

Mikhailova, V. A. ^{[1
]}

Popov, V. V. ^{[1
,2
]}

Sergienko, E. S. ^{[2
]}

Danilova, A., V ^{[1
]}

Otmas, N. M. ^{[1
]}

Zhuravlev, A., V ^{[3
]}

机构：

[1] All Russia Petr Res Explorat Inst VNIGRI, St Petersburg, Russia

[2] St Petersburg State Univ, St Petersburg, Russia

[3] Russian Acad Sci, Komi Sci Ctr, Inst Geol, Ural Branch, Syktyvkar, Russia

[4] Inst Terr Magnetism Ionosphere & Radiowave, St Petersburg Branch, St Petersburg, Russia

来源：

RECENT ADVANCES IN ROCK MAGNETISM, ENVIRONMENTAL MAGNETISM AND PALEOMAGNETISM | 2019年

基金：

俄罗斯基础研究基金会;

关键词：

Carboniferous deposits; Paleomagnetic poles; Russian platform;

D O I：

10.1007/978-3-319-90437-5_4

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

New results for the Carboniferous rocks (Moscovian, Bashkirian and Visean stages) from four sections of the Russian Platform are presented. Primary magnetite and secondary hematite are the main carriers of magnetization in the studied rocks. All isolated NRM components generally correspond to the geomagnetic field of reversed polarity. Only in the rocks of the Visean stage a small zone of normal polarity is found. Widespread late Paleozoic remagnetization of the Carboniferous rocks of the Russian Platform is detected.

引用

页码：37 / 54

页数：18

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