Evolution of the Subsurface K-Rich Brines in the Triassic Carbonates in the Sichuan Basin of China-Reference-Cited by-同舟云学术

Evolution of the Subsurface K-Rich Brines in the Triassic Carbonates in the Sichuan Basin of China

Author:

Zhou Xun¹²,Wang Xiaocui¹³,Han Jiajun¹⁴,Cao Qin¹⁵,Jiang Changlong¹⁶,Guo Juan¹,Zhou Haiyan⁷

Affiliation:

1. School of Water Resources and Environment; China University of Geosciences (Beijing); Xueyuan Road 29, Beijing 100083 P. R. China

2. MOE Laboratory of Groundwater Circulation and Evolution; China University of Geosciences (Beijing); Xueyuan Road 29, Beijing 100083 P. R. China

3. School of Environmental Science and Engineering; Qingdao University; Ningxia Road 308, Qingdao Shandong 266071 P. R. China

4. Beijing Guodaotong Highway Design & Research Institute CO., LTD; Huaibaishuhou Street 23, Beijing 100053 P. R. China

5. Education Centre of Jiangxi Geological Exploration Bureau; Nanchang Jiangxi 330030 P. R. China

6. Songliao Water Resources Commission (SWRC); No. 4188 Jiefang Road, Changchun, Jilin 130021 P. R. China

7. Subsurface Insights; Hanover NH 03755

Funder

Project from Chinese Geological Survey

National Key Project of Foundational Research and Development of China (973 Project)

National Natural Science Foundation of China

Publisher

Wiley

Subject

Computers in Earth Sciences,Water Science and Technology

Link

Reference49 articles.

5. Origin and chemical evolution of brines in sedimentary basins;Carpenter;Oklahoma Geological Survey Circular,1978

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