南海北部边缘盆地泥底辟及泥火山特征及其与油气运聚关系

何家雄; 祝有海; 翁荣南; 崔莎莎

doi:10.3799/dqkx.2010.008

Volume 35 Issue 1

Jan. 2010

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Article Navigation > Earth Science > 2010 > 35(1): 75-86

HE Jia-xiong, ZHU You-hai, WENG Jung-nan, CUI Sha-sha, 2010. Characters of North-West Mud Diapirs Volcanoes in South China Sea and Relationship between Them and Accumulation and Migration of Oil and Gas. Earth Science, 35(1): 75-86. doi: 10.3799/dqkx.2010.008

Citation:

HE Jia-xiong, ZHU You-hai, WENG Jung-nan, CUI Sha-sha, 2010. Characters of North-West Mud Diapirs Volcanoes in South China Sea and Relationship between Them and Accumulation and Migration of Oil and Gas. Earth Science, 35(1): 75-86. doi: 10.3799/dqkx.2010.008

Citation:

HE Jia-xiong, ZHU You-hai, WENG Jung-nan, CUI Sha-sha, 2010. Characters of North-West Mud Diapirs Volcanoes in South China Sea and Relationship between Them and Accumulation and Migration of Oil and Gas. Earth Science, 35(1): 75-86. doi: 10.3799/dqkx.2010.008

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Characters of North-West Mud Diapirs Volcanoes in South China Sea and Relationship between Them and Accumulation and Migration of Oil and Gas

doi: 10.3799/dqkx.2010.008

1.
Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
2.
Institute of Mineral Resources, Chinese Academy of Geological Seiences, Beijing 100037, China
3.
Chinese Petroleum Corp., Exploration & Production Business Division, Taipei 11010, China

Received Date: 2009-07-26
Publish Date: 2010-01-01

Abstract

Abstract

It has geological and mode of occurrence differences between mud diapirs and mud volcanoes though the similar genesis and the characters of evolution and development. Mud diapirs in Yinggehai basin located in the central deep depression, appeared on five north-west lines and had characters of low density, low wave velocity, high temperature and high pressure however mud volcanoes in Southwest Taiwan basin located in the continental deep-water distract in the south depression and Tainan-Kaohsiung distract in Taiwan. It located along the discordogenic fault and usually had calderas also sea floors. Mud diapirs and mud volcanoes had many styles of accompanying gas to be mainly of the mature-post mature coaliferous gas and had abundence CO² and N² to be mainly of the inorganic-crustal CO². The mud formations were Miocene and Pliocene marine mud shales which was souce rocks, furthermore it made a effictive system with the channel and affiliated structures generated by mud diapirs and mud volcanoes, so it was a particular petroleum system controlling the distribution of oil and gas.
- Yinggehai basin,
- Southwest Taiwan basin,
- mud diapirs/mud volcanoes,
- geology and geophysics,
- oil-gas accumulation and migration characters

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References(65)

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Characters of North-West Mud Diapirs Volcanoes in South China Sea and Relationship between Them and Accumulation and Migration of Oil and Gas

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