渤南洼陷流体包裹体特征与成藏期流体压力恢复

刘华; 蒋有录; 卢浩; 刘雅利; 景琛

doi:10.3799/dqkx.2016.109

Volume 41 Issue 8

Aug. 2016

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Article Navigation > Earth Science > 2016 > 41(8): 1384-1394

Liu Hua, Jiang Youlu, Lu Hao, Liu Yali, Jing Chen, 2016. Restoration of Fluid Pressure during Hydrocarbon Accumulation Period and Fluid Inclusion Feature in the Bonan Sag. Earth Science, 41(8): 1384-1394. doi: 10.3799/dqkx.2016.109

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Liu Hua, Jiang Youlu, Lu Hao, Liu Yali, Jing Chen, 2016. Restoration of Fluid Pressure during Hydrocarbon Accumulation Period and Fluid Inclusion Feature in the Bonan Sag. Earth Science, 41(8): 1384-1394. doi: 10.3799/dqkx.2016.109

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Restoration of Fluid Pressure during Hydrocarbon Accumulation Period and Fluid Inclusion Feature in the Bonan Sag

doi: 10.3799/dqkx.2016.109

Liu Hua^{1,2
,},
Jiang Youlu^1,2,
Lu Hao³,
Liu Yali³,
Jing Chen^1,2

1.
School of Geosciences, China University of Petroleum, Qingdao 266580, China
2.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
3.
Exploration and Development Research Institute, Shengli Oilfield Company Limited SINOPEC, Dongying 257000, China

Received Date: 2016-01-30
Publish Date: 2016-08-15

Abstract

Abstract

Bonan sag is rich in oil and gas resources, yet its complicated accumulation process results in a poor understanding of its dynamic conditions during hydrocarbon accumulation. In this study, the fluid pressure in the hydrocarbon accumulation period was recovered in the Bonan sag using such fluid inclusion analysis techniques as microscopic fluorescence, homogenization temperature and freezing point. The results show that the fluorescence of hydrocarbon inclusions in Es₃ Member reservoir is yellow-white, and yellow-green, and the homogenization temperatures of fluid inclusions are 80-130 ℃, indicating that hydrocarbons were accumulated during the period from the middle and late stage of Minghuazhen Formation deposition to present. Whereas the fluorescence of hydrocarbon inclusions in the Es₄ Member reservoirs is yellow, yellow-green and blue-green, and the homogenization temperatures of fluid inclusions are 70-80 ℃ and 90-130 ℃, corresponding to the two stages of hydrocarbon accumulation, namely the Dongying stage and the early stage of Minghuazhen to present, of which the latter is dominant. Meanwhile, reservoirs were generally with abnormal pressure in the period of hydrocarbon accumulation on a large scale. In the first period of hydrocarbon charging, the hydrocarbon generation was limited with the weak pressure coefficient, but in the second period of hydrocarbon charging, due to a large amount of hydrocarbons generated by the matured source rocks, the abnormal pressure gradually increased, the overpressure area enlarged, and the formation pressure coefficient reached 1.80. The overpressure could have provided sufficient driving force, and affected the directions of hydrocarbon migration and accumulation.
- fluid inclusion,
- homogenization temperature,
- hydrocarbon accumulation stage,
- driving force of hydrocarbon migration,
- abnormal overpressure,
- Bonan sag,
- petroleum geology,

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References(59)

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Restoration of Fluid Pressure during Hydrocarbon Accumulation Period and Fluid Inclusion Feature in the Bonan Sag

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