下诺夫哥罗德地区东欧地台韦特卢加河下游二叠纪-三叠纪界线的磁地层学

A. Fetisova, R. Veselovskiy, V. K. Golubev, M. Arefiev
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引用次数: 0

摘要

我们介绍了对东欧地台中部位于韦特卢加河下游的六个二叠纪-三叠纪边界断面进行详细古地磁研究的结果:它们是:Astashikha、Voskresenskoe、Znamenskoe、Prudovka、Sosnovka 和 Sukhoborka。符合现代实验室处理质量标准的古地磁数据与生物地层学研究结果一起,为每个地段制定和证实了磁地层尺度,以及它们之间的相互关系,并为韦特卢加河二叠纪-三叠纪沉积复合体构建了磁极尺度。确定了每个研究地段的岩磁特征,并计算了晚二叠世和二叠-三叠世边界的东欧地台古磁极。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Magnetostratigraphy of the Permian–Triassic Boundary in the Lower Reaches of the Vetluga River, East European Platform, Nizhny Novgorod Region
We present the results of detailed paleomagnetic studies of six Permian-Triassic boundary sections in the central part of the East European Platform, located in the lower reaches of the Vetluga River: Astashikha, Voskresenskoe, Znamenskoe, Prudovka, Sosnovka, and Sukhoborka. The paleomagnetic data, which meet the modern quality standards for laboratory processing, together with the results of biostratigraphic studies, allow for the development and substantiation of magnetostratigraphic scales for each section, as well as for their correlation and the construction of a magnetic polarity scale for the Permian-Triassic sedimentary complex of the Vetluga River. Rock-magnetic characteristics are determined for each of the studied sections, and paleomagnetic poles of the East European Platform are calculated for the Late Permian and Permian-Triassic boundary.
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