刻赤-塔曼地区塞米戈尔斯基、安德鲁索夫和博鲁克-奥巴泥质火山粘土浆中的有孔虫

IF 0.3 Q4 GEOLOGY

Moscow University Geology Bulletin Pub Date : 2024-06-05 DOI:10.3103/s0145875224700042

E. M. Bugrova, M. R. Latypova, L. F. Kopaevich, A. V. Gusev

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引用次数: 0

摘要

摘要根据塞米戈尔斯基、安德鲁索夫和博鲁克-奥巴泥火山粘土浆中的有孔虫集合体，完善了刻赤-塔曼地区的地层学。通过与贝拉亚河（阿迪盖亚共和国）沿岸古新世参考地段的动物群进行比较，我们发现了中始新世（卢泰期和巴顿期的切尔克斯克地层和库马地层）、下渐新世（鲁佩利期的普谢卡地层）（通过发现翼足目动物遗骸得到证实）和中新世（中新世东帕拉特提斯地区尺度的康基期和萨尔马特期）的沉积物。白垩纪沉积物（塞米戈尔斯基火山）被认为是晚坎帕尼亚期-马斯特里赫特期的产物。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Foraminifera from Clay Pulp of the Semigorsky, Andrusov, and Borukh-Oba Mud Volcanoes in the Kerch–Taman Region

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Foraminifera from Clay Pulp of the Semigorsky, Andrusov, and Borukh-Oba Mud Volcanoes in the Kerch–Taman Region

Abstract

The stratigraphy of the Kerch–Taman region has been refined based on foraminiferal assemblages from the clay pulp of the Semigorsky, Andrusov, and Borukh-Oba mud volcanoes. Comparison with the fauna from the reference section of the Paleogene along the Belaya River (Republic of Adygea) enabled us to reveal deposits of the Middle Eocene (Cherkessk and Kuma formations of the Lutetian and Bartonian stages); Lower Oligocene (Pshekha Formation, Rupelian Stage), confirmed by finds of remains of pteropods; and Middle Miocene (Konkian and Sarmatian stages of the Eastern Paratethys regional scale of the Miocene). Cretaceous deposits (Semigorsky Volcano) are attributed to the Late Campanian–Maastrichtian.

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来源期刊

Moscow University Geology Bulletin GEOLOGY-

CiteScore

0.60

自引率

25.00%

发文量

期刊介绍： Moscow University Geology Bulletin is the journal that mainly publishes scientific articles, short reports of graduate students, and reviews. Publications made by the members of the Faculty of Geology of the Moscow State University and their collaborators are published. Publications encompass all branches of geology.