Email this article Clay Mineral Complexes of the Quaternary Sediments in the Canyon–Cone System of the Shakhe River (Black Sea)
- Authors: Ye Yuanqiu 1, Luksha V.L.1
-
Affiliations:
- Department of Geology, Moscow State University
- Issue: Vol 74, No 2 (2019)
- Pages: 229-232
- Section: Short Communications
- URL: https://journals.rcsi.science/0145-8752/article/view/174959
- DOI: https://doi.org/10.3103/S0145875219020133
- ID: 174959
Cite item
Open Access
Access granted
Subscription Access
Abstract
The distribution features of clay minerals in the Quaternary sediments are considered in the canyon–deepwater cone sedimentary system of the Shakhe River in the Black Sea. The ratio of illite, chlorite, smectite, and kaolinite that occurs along the area and section is based on the transfer of sedimentary material by turbidity flows through the canyon with the formation of a unified mineralogical province.
Keywords
About the authors
Ye Yuanqiu
Department of Geology, Moscow State University
Author for correspondence.
Email: rachel.ye@mail.ru
Russian Federation, Moscow, 119234
V. L. Luksha
Department of Geology, Moscow State University
Email: rachel.ye@mail.ru
Russian Federation, Moscow, 119234
