Hydrothermal alteration and corresponding reservoir significance of the Permian Emeishan basaltic lavas, west Sichuan, China

Author:

Sun Y. B.1ORCID,Zhang Y. F.12ORCID,Xi A. H.1,Tang Y.1,Zhang B. J.3,Pei S. Q.4,Li R. R.4,Yin H.4,Zeng Q.4,Qu H. Z.12,Zhou R. J.5

Affiliation:

1. School of Geoscience and Technology, Southwest Petroleum University, Chengdu, China

2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu, China

3. Exploration and Development Research Institute, PetroChina Southwest Oil and Gas Field Company, Chengdu, China

4. Branch of Chuanxibei Gas Field, PetroChina Southwest Oil and Gas Field Company, Jiangyou, China

5. School of Earth and Environmental Sciences, The University of Queensland, St Lucia, Australia

Funder

National Natural Science Foundation of China

Publisher

Informa UK Limited

Subject

General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)

Reference46 articles.

1. Emeishan large igneous province (SW China) and the mantle-plume up-doming hypothesis

2. Applying X-Ray Geothermometer Diffraction to a Chlorite

3. Bureau of Geology and Mineral Resources of Sichuan Province (1991). Regional geology of Sichuan Province (pp. 310–440). Geological Publishing House. (in Chinese with English abstract)

4. A chlorite solid solution geothermometer the Los Azufres (Mexico) geothermal system

5. Groundwater contamination in mega cities with finite sources

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