旧石器时代和磁层描记俄罗斯板块中心点:沟渠、斯卢基诺和奥克会议

А. М. Фетисова, В. К. Голубев, Р. В. Веселовский, Ю.П. Балабанов
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引用次数: 0

摘要

本文介绍了在东欧地台中部朱可夫-奥夫拉格、斯鲁金诺和奥克斯基-赛兹德三个二叠纪-三叠纪大陆红层参考剖面上进行的详细磁地层学研究结果。更新了俄罗斯盆地二叠纪—三叠纪的磁地层尺度。结果表明,R3P磁带的组成很可能不是以前假设的4个亚带,而是5个亚带
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ПАЛЕОМАГНЕТИЗМ И МАГНИТОСТРАТИГРАФИЯ ОПОРНЫХ ПЕРМО-ТРИАСОВЫХ РАЗРЕЗОВ ЦЕНТРАЛЬНОЙ ЧАСТИ РУССКОЙ ПЛИТЫ: ЖУКОВ ОВРАГ, СЛУКИНО И ОКСКИЙ СЪЕЗД
We present the results of detailed magnetostratigraphic studies, carried out on three reference Permian-Triassic sections of continental red beds in the central part of the East European platform – Zhukov Ovrag, Slukino and Okskiy Syezd. The magnetostratigraphic scale of the Permian-Triassic interval of the Russian basin has been updated. It is shown that the composition of the R3P magnetozone most likely includes not 4 subzones, as it was assumed before, but 5
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