雪峰山前陆盆地下志留统页岩气勘探潜力

刘辰生; 郭建华; 王宗秀

doi:10.3799/dqkx.2019.208

Volume 44 Issue 11

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(11): 3678-3691

Liu Chensheng, Guo Jianhua, Wang Zongxiu, 2019. Potential for Shale Gas Exploration of Xuefengshan Foreland Basin of Lower Silurian. Earth Science, 44(11): 3678-3691. doi: 10.3799/dqkx.2019.208

Citation:

Liu Chensheng, Guo Jianhua, Wang Zongxiu, 2019. Potential for Shale Gas Exploration of Xuefengshan Foreland Basin of Lower Silurian. Earth Science, 44(11): 3678-3691. doi: 10.3799/dqkx.2019.208

Liu Chensheng, Guo Jianhua, Wang Zongxiu, 2019. Potential for Shale Gas Exploration of Xuefengshan Foreland Basin of Lower Silurian. Earth Science, 44(11): 3678-3691. doi: 10.3799/dqkx.2019.208

Citation:

Liu Chensheng, Guo Jianhua, Wang Zongxiu, 2019. Potential for Shale Gas Exploration of Xuefengshan Foreland Basin of Lower Silurian. Earth Science, 44(11): 3678-3691. doi: 10.3799/dqkx.2019.208

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Potential for Shale Gas Exploration of Xuefengshan Foreland Basin of Lower Silurian

doi: 10.3799/dqkx.2019.208

Liu Chensheng^{1,2,3
,
,},
Guo Jianhua^1,2,3,
Wang Zongxiu⁴

1.
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083, China
2.
Key Laboratory of Non-Ferrous Resources and Geological Hazard Detection of Hunan Province, Changsha 410083, China
3.
School of Geosciences and Info-Physics, Central South University, Changsha 410083, China
4.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

Received Date: 2019-08-25
Publish Date: 2019-11-15

Abstract

Abstract

The Xuefengshan Silurian foreland basin is located in the Central-Northwest Hunan-Sichuan basin, which is the main basin type of the Upper Yangtze plate. Sedimentary formation process and shale gas exploration potential of foreland basins in Northwest and Central Hunan are analyzed based on field data, logging data and testing data. The facies of foredeep include turbidite fan and shelf. Facies of back bulge basin include tidal flat, shelf, shore, delta and carbonate platform facies and so on. So, facies in back bulge basin are more abundant than in foredeep. Though the facies are different greatly in foredeep and back bulge basin, the sedimentary cycles in those systems are coherent. So foredeep and back bulge basin are connected and Xuefengshan obstructing is limited for the foredeep and back bulge basin distributed around Xufengshan. Based on geochemistry data and analysis data, TOC and organic matter type in study area are poorer than in Jiaoshiba area in Sichuan basin. Based on regional section correlation, black carbonaceous shale distributed at the bottom of Longmaxi Formation is absent in the study, causing TOC and organic matter type being poorer than in Jiaoshiba. The main reason for the poor geochemical indexes of Silurian shale in Hunan is the lack of black carbonaceous shale in the first cycle of Longmaxi Formation.
- Yangtze plate,
- foreland basin,
- Silurian,
- carbonaceous shale,
- Jiaoshiba,
- petroleum geology

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Potential for Shale Gas Exploration of Xuefengshan Foreland Basin of Lower Silurian

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