A Buried Landslide Block in a Section of Middle Jurassic Deposits in the Moscow Region
- Authors: Alekseev A.S.1, Gabdullin R.R.1, Samarin E.N.1, Zerkal O.V.1, Rostovtsteva J.I.1
-
Affiliations:
- Department of Geology, Moscow State University
- Issue: Vol 74, No 4 (2019)
- Pages: 357-363
- Section: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/175007
- DOI: https://doi.org/10.3103/S0145875219040021
- ID: 175007
Cite item
Abstract
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.
Keywords
About the authors
A. S. Alekseev
Department of Geology, Moscow State University
Author for correspondence.
Email: aaleks@geol.msu.ru
Russian Federation, Moscow, 119991
R. R. Gabdullin
Department of Geology, Moscow State University
Author for correspondence.
Email: mosgorsun@rambler.ru
Russian Federation, Moscow, 119991
E. N. Samarin
Department of Geology, Moscow State University
Author for correspondence.
Email: samarinen@mail.ru
Russian Federation, Moscow, 119991
O. V. Zerkal
Department of Geology, Moscow State University
Author for correspondence.
Email: igzov@mail.ru
Russian Federation, Moscow, 119991
Ju. I. Rostovtsteva
Department of Geology, Moscow State University
Author for correspondence.
Email: paleopen@mail.ru
Russian Federation, Moscow, 119991