Clay Mineral Complexes of the Quaternary Sediments in the Canyon–Cone System of the Shakhe River (Black Sea)
- 作者: Ye Yuanqiu 1, Luksha V.1
-
隶属关系:
- Department of Geology, Moscow State University
- 期: 卷 74, 编号 2 (2019)
- 页面: 229-232
- 栏目: Short Communications
- URL: https://journals.rcsi.science/0145-8752/article/view/174959
- DOI: https://doi.org/10.3103/S0145875219020133
- ID: 174959
如何引用文章
详细
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.
作者简介
Ye Yuanqiu
Department of Geology, Moscow State University
编辑信件的主要联系方式.
Email: rachel.ye@mail.ru
俄罗斯联邦, Moscow, 119234
V. Luksha
Department of Geology, Moscow State University
Email: rachel.ye@mail.ru
俄罗斯联邦, Moscow, 119234