A Buried Landslide Block in a Section of Middle Jurassic Deposits in the Moscow Region
- Авторлар: Alekseev A.1, Gabdullin R.1, Samarin E.1, Zerkal O.1, Rostovtsteva J.1
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Мекемелер:
- Department of Geology, Moscow State University
- Шығарылым: Том 74, № 4 (2019)
- Беттер: 357-363
- Бөлім: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/175007
- DOI: https://doi.org/10.3103/S0145875219040021
- ID: 175007
Дәйексөз келтіру
Аннотация
A section of Upper Carboniferous and overlying Jurassic sediments in the area of a buried karst depression in the northwestern part of Moscow was studied. According to conodont zoning, it was revealed that in the section of the karst depression the Perkhur Formation directly lies on the Voskresensk Formation altered by karst processes. It was shown that the absence of the Neverovo Formation in the section is associated with landslide deformations, which occurred in the Middle Jurassic (Kudinovo) time, that is, the movement of a block of the Perkhurovsky limestones, which was located hypersometrically higher on the slope of the karst paleodepression.
Негізгі сөздер
Авторлар туралы
A. Alekseev
Department of Geology, Moscow State University
Хат алмасуға жауапты Автор.
Email: aaleks@geol.msu.ru
Ресей, Moscow, 119991
R. Gabdullin
Department of Geology, Moscow State University
Хат алмасуға жауапты Автор.
Email: mosgorsun@rambler.ru
Ресей, Moscow, 119991
E. Samarin
Department of Geology, Moscow State University
Хат алмасуға жауапты Автор.
Email: samarinen@mail.ru
Ресей, Moscow, 119991
O. Zerkal
Department of Geology, Moscow State University
Хат алмасуға жауапты Автор.
Email: igzov@mail.ru
Ресей, Moscow, 119991
Ju. Rostovtsteva
Department of Geology, Moscow State University
Хат алмасуға жауапты Автор.
Email: paleopen@mail.ru
Ресей, Moscow, 119991