东欧地台下诺夫哥罗德地区韦特卢加河下游二叠纪-三叠纪界线的磁地层学

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Izvestiya, Physics of the Solid Earth Pub Date : 2024-07-18 DOI:10.1134/s1069351324700460
A. M. Fetisova, R. V. Veselovskiy, V. K. Golubev, M. P. Arefiev
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引用次数: 0

摘要

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:这些地段位于维特卢加河下游: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,加上生物地层学研究的结果,使我们有可能为每个地段制定和证实磁地层尺度,并将它们关联起来,为韦特卢加河二叠纪-三叠纪沉积复合体编制综合磁极尺度。确定了每个研究地段的岩石磁性特征,并计算了晚二叠世和二叠-三叠世边界的东欧地台古磁极。
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Magnetostratigraphy of the Permian–Triassic Boundary in the Lower Reaches of the Vetluga River, Nizhny Novgorod Region, East European Platform

Abstract—We present the results of detailed paleomagnetic studies of six Permian–Triassic boundary sections in the central part of the East European Platform, which are 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, make it possible to develop and substantiate the magnetostratigraphic scales for each section, as well as to correlate them and to compile a composite 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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来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
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