Collapse-Breccia as a Sign of the Pre-Existing Evaporites (Lower Riphean Satka Suite, South Ural

The presence of pre-existing evaporites in the carbonate unit is considered on example of the Lower Riphean Satka Suite. It is proved by the extensive development of the collapse breccia in the Karagay member of the Upper Satka subsuite. The difference of collapse-breccias from other sedimentary bre...

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Bibliographic Details
Main Author: M. T. Krupenin
Format: Article
Language:English
Published: Perm Sate National Research University 2018-12-01
Series:Vestnik Permskogo Universiteta: Seriâ Geologiâ
Subjects:
Online Access:http://geology-vestnik.psu.ru/index.php/geology/article/view/270