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Volume 46 Issue 1
Jan.  2024
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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2024  >  46(1): 111-123
XU Qinqi, CHU Chenglin, GUO Xiaowen, LIU Yongli, ZHANG Li, LUO Mingxia. Geochemical characteristics of crude oil and contributions to hydrocarbon accumulation in multiple stages in Tahe subsalt area[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2024, 46(1): 111-123. doi: 10.11781/sysydz202401111
Citation: XU Qinqi, CHU Chenglin, GUO Xiaowen, LIU Yongli, ZHANG Li, LUO Mingxia. Geochemical characteristics of crude oil and contributions to hydrocarbon accumulation in multiple stages in Tahe subsalt area[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2024, 46(1): 111-123. doi: 10.11781/sysydz202401111
shu

Geochemical characteristics of crude oil and contributions to hydrocarbon accumulation in multiple stages in Tahe subsalt area

doi: 10.11781/sysydz202401111
  • 1.

    Research Institute of Exploration and Production, SINOPEC Northwest Oilfield Branch Company, Urumqi, Xinjiang 830011, China

  • 2.

    Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

  • 3.

    Faculty of Earth Resources, China University of Geosciences (Wuhan), Wuhan, Hubei 430074, China

  • Received Date: 2023-04-27
  • Rev Recd Date: 2024-01-03
  • Publish Date: 2024-01-28
    Abstract
  • The process of hydrocarbon accumulation in polycyclic superimposed basins often involves multistage crude oil charging, but not every stage of crude oil charging plays a significant role in the current hydrocarbon accumulation. Fluid inclusion methods can only provide constraints on the stages and time of crude oil charging, but cannot determine the contribution of each stage of crude oil charging for hydrocarbon accumulation. To study the contributions of different stages of crude oil charging for the reservoirs, the Ordovician carbonate reservoirs in the subsalt area, Tahe oilfield (Tahe subsalt area) were taken as an example. This study employed crude oil geochemistry, fluid inclusion analysis, fluorescence spectrum, and single well simulation analysis methods to systematically reveal the fluorescence characteristics of crude oil and hydrocarbon accumulation stages and time of the study area. The analysis of crude oil biomarker parameters indicates that the crude oil has the same parent material and was deposited in a marine weak reducing environment. By comparing the crude oil with the study area's source rocks, it was determined that all the crude oil was derived from the source rocks of the Lower Cambrian Yuertusi Formation. The aromatic methylphenanthrene index and methyldibenzothiophene parameters of crude oil serve as effective indicators for the quantitative evaluation of crude oil maturity. The calculated crude oil maturity (Ro) in the Tahe subsalt area ranges from 0.90% to 1.47%, and this may correspond to multiple stages of oil and gas charging. Based on fluorescence spectrum analysis of oil inclusions and homogeneity temperature and salinity measurements of associated saline inclusions in the Ordovician reservoirs in the Tahe subsalt area and the study area's burial history of single well burial history and thermal history simulation, it was determined that the oil reservoirs in the Tahe subsalt area experienced three stages of crude oil charging during the stages of middle Caledonian (420 Ma), middle Hercynian (318 Ma) and late Himalayan (10 Ma). By comparing the fluorescence spectrum parameters of crude oil and oil inclusions in these three stages, it is concluded that the late Himalayan is the primary stage of hydrocarbon accumulation in the Tahe subsalt area, making the largest contribution for the Ordovician reservoirs in the Tahe subsalt area.

     

    • All authors disclose no relevant conflict of interests.
    The study was designed by XU Qinqi and LIU Yongli. The experimental operation was completed by GUO Xiaowen, CHU Chenglin and LUO Mingxia. The manuscript was drafted and revised by XU Qinqi, GUO Xiaowen and ZHANG Li. All the authors have read the last version of paper and consented for submission.
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