Volume 44 Issue 3
May  2022
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WANG Yang, ZHANG Shaonan, LIU Yongli. Controls of strike-slip fault activities on hydrocarbon accumulation in Tahe Oilfield, Tarim Basin: a case study of TP 39 fault zone[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(3): 394-401. doi: 10.11781/sysydz202203394
Citation: WANG Yang, ZHANG Shaonan, LIU Yongli. Controls of strike-slip fault activities on hydrocarbon accumulation in Tahe Oilfield, Tarim Basin: a case study of TP 39 fault zone[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2022, 44(3): 394-401. doi: 10.11781/sysydz202203394

Controls of strike-slip fault activities on hydrocarbon accumulation in Tahe Oilfield, Tarim Basin: a case study of TP 39 fault zone

doi: 10.11781/sysydz202203394
  • Received Date: 2021-10-25
  • Rev Recd Date: 2022-04-20
  • Publish Date: 2022-05-28
  • Strike-slip faults were well-developed in the Tahe Oilfield, Tarim Basin, which had an important control to the accumulation and distribution of hydrocarbon. In this study, the TP 39 strike-slip fault in the Tahe Oilfield was taken as an example, fluid inclusions were used to determine the time of hydrocarbon charge based on the analysis of strike-slip fault activity history, and the relationship between hydrocarbon charging events and fault activity history was studied. Results show that the TP 39 strike-slip fault zone is rich in oil and gas resources and has the characteristics of multi-stage activities, namely the Middle-Late Caledonian to Early Hercynian, Indosinian and Yanshanian-Himalayan, respectively. The results of fluid inclusion analysis indicated that there were four episodes of oil charge to the Ordovician reservoir of TP 39 strike-slip fault, and oil inclusions with golden-yellowish, yellow, yellow-green and blue fluorescing colors were trapped. According to the minimum homogenization temperature of aqueous inclusions co-existed with oil-bearing inclusions, combined with the burial and thermal histories of reservoirs, there were four periods of oil filling events occurred at around 440, 324, 220 and 110 Ma, corresponding to Caledonian, Hercynian, Indosinian and Yanshanian, respectively, which showed a good response relationship with the fault activity time. It was then concluded that the activities of strike-slip fault constrained the time of hydrocarbon charge, thus controlled the whole process of hydrocarbon accumulation.

     

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