塔里木盆地哈拉哈塘凹陷奥陶系成藏流体演化

肖晖; 赵靖舟; 杨海军; 蔡振忠; 朱永峰; 高莲花; 张妮

doi:10.3799/dqkx.2012.S1.016

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Article Navigation > Earth Science > 2012 > 37(S1): 163-173

XIAO Hui, ZHAO Jing-zhou, YANG Hai-jun, CAI Zhen-zhong, ZHU Yong-feng, GAO Lian-hua, ZHANG Ni, 2012. Fluid Inclusion and Micro-FTIR Evidence for Hydrocarbon Charging Fluid Evolution of the Ordovician Reservoir of Halahatang Depression, the Tarim Basin. Earth Science, 37(S1): 163-173. doi: 10.3799/dqkx.2012.S1.016

Citation:

XIAO Hui, ZHAO Jing-zhou, YANG Hai-jun, CAI Zhen-zhong, ZHU Yong-feng, GAO Lian-hua, ZHANG Ni, 2012. Fluid Inclusion and Micro-FTIR Evidence for Hydrocarbon Charging Fluid Evolution of the Ordovician Reservoir of Halahatang Depression, the Tarim Basin. Earth Science, 37(S1): 163-173. doi: 10.3799/dqkx.2012.S1.016

Citation:

XIAO Hui, ZHAO Jing-zhou, YANG Hai-jun, CAI Zhen-zhong, ZHU Yong-feng, GAO Lian-hua, ZHANG Ni, 2012. Fluid Inclusion and Micro-FTIR Evidence for Hydrocarbon Charging Fluid Evolution of the Ordovician Reservoir of Halahatang Depression, the Tarim Basin. Earth Science, 37(S1): 163-173. doi: 10.3799/dqkx.2012.S1.016

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Fluid Inclusion and Micro-FTIR Evidence for Hydrocarbon Charging Fluid Evolution of the Ordovician Reservoir of Halahatang Depression, the Tarim Basin

doi: 10.3799/dqkx.2012.S1.016

1.
School of Petroleum Resources, Xi'an Shiyou University, Xi'an 710065, China
2.
Key Laboratory of Hydrocarbon Accumulation, School of Petroleum Resources, Xi'an Shiyou University, Xi'an 710065, China
3.
Petrochina Tarim Oilfield Company, Kuerle 841000, China

Received Date: 2011-11-08
Available Online: 2021-11-15
Publish Date: 2012-05-01

Abstract

Abstract

The evolution of the hydrocarbon charging fluids of the Ordovician reservoir, Halahatang depression and the Tarim basin, was studied by the evidence of inclusion petrography, transmitted light-incident fluorescence, homogenization temperature and Micro-FTIR of the petroleum inclusions. The experiments data show that: firstly, two hydrocarbon charging stages were determined, the peak homogenization temperature of associated saline inclusions were 72.5-78.5 ℃ and 92.1-99.7 ℃ respectively; secondly, the Micro-FTIR data confirm that there generally exist H₂O in the petroleum inclusion; furthermore, the ratio of H₂O/(CH₂+CH₃) in the primary hydrocarbon inclusions is larger (4.6-2.1) than the ratio (1.1-0.4) in the secondary hydrocarbon inclusions, and the maturity of the primary hydrocarbon inclusions (CH₂/CH₃ ratio is 7.3-4.5) is lower than the maturity of the secondary hydrocarbon inclusions (CH₂/CH₃ ratio is 2.9-1.9); lastly, sulf-alcohols compounds generally exist in the primary hydrocarbon inclusions, but do not exist in the secondary hydrocarbon inclusions. Compared with geochemistry data of the Ordovician hydrocarbon, sulf-alcohols compounds were the product of the early reservoir biodegradation having occurred in early-Hercynian, and in the late-Hercynian, the higher maturity hydrocarbon largely generated charges and mixes with the early hydrocarbon, which causes the content of the sulf-alcohols decreased. At the same time, part of the sulf-alcohols cracks to generate H₂S.
- inclusion,
- Micro-FTIR,
- charging fluid,
- Halahatang depression,
- geochemistry,
- hydrocarbon

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References(88)

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沈阳化工大学材料科学与工程学院沈阳 110142

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Fluid Inclusion and Micro-FTIR Evidence for Hydrocarbon Charging Fluid Evolution of the Ordovician Reservoir of Halahatang Depression, the Tarim Basin

doi: 10.3799/dqkx.2012.S1.016

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