The Carboniferous of the Moscow syneclise: Paleomagnetic data

被引:1
|
作者
Iosifidi, A. G. [1 ,3 ]
Mikhailova, V. A. [1 ]
Popov, V. V. [1 ,2 ]
Sergienko, E. S. [2 ]
Danilova, A. V. [1 ]
Otmas, N. M. [1 ]
机构
[1] All Russia Petr Res Explorat Inst VNIGRI, St Petersburg 191014, Russia
[2] St Petersburg State Univ, St Petersburg 199034, Russia
[3] Inst Terr Magnetism Ionosphere & Radiowave Propag, St Petersburg Branch, St Petersburg 191023, Russia
基金
俄罗斯基础研究基金会;
关键词
Carboniferous deposits; paleomagnetic poles; Russian Platform; PLATFORM;
D O I
10.1134/S1069351318010081
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 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.
引用
收藏
页码:163 / 177
页数:15
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