Article ; Online: Geological Characteristics of Lower Paleozoic Shale Gas Accumulation in the Yuxi Region, Southern Sichuan Basin: In View of High-Density Methane Inclusions.
ACS omega
2022 Volume 7, Issue 31, Page(s) 27422–27435
Abstract: ... 4200 m in three wells located in different tectonic zones in the Yuxi Region, southern Sichuan Basin ... veins of the Wufeng-Longmaxi Formation in the Yuxi Region are mainly formed vertically and horizontally ...
Abstract | Twelve shale fracture veins and forty-nine fluid inclusion assemblages within the veins of 3800-4200 m in three wells located in different tectonic zones in the Yuxi Region, southern Sichuan Basin were selected in this study. The burial and thermal histories of single wells were reconstructed, and time-temperature-pressure of oil and gas filling were clarified using microscopy observation, Raman microprobe analyses, geochemical tests, and fluid inclusion microtemperature measurement. The shale fracture veins of the Wufeng-Longmaxi Formation in the Yuxi Region are mainly formed vertically and horizontally, where the vein-forming fluids are derived from endogenous fluids. A large number of methane inclusions, bituminous inclusions, and methane-bearing bituminous inclusions within the veins confirm the process of oil cracking gas and kerogen cracking gas. The homogeneous temperature (Th) of the aqueous inclusions contemporaneous with the bituminous inclusions ranges from 109.3 to 174.1 °C, which were trapped during 220 to 250 Ma. The homogeneous temperature of the aqueous inclusions contemporaneous with the methane inclusions ranges from 137.3 to 226.8 °C, which were trapped during 160 to 195 Ma and 51 to 56 Ma. The trapped pressure calculated by high-density methane inclusions (0.246-0.293 g/cm |
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Language | English |
Publishing date | 2022-07-27 |
Publishing country | United States |
Document type | Journal Article |
ISSN | 2470-1343 |
ISSN (online) | 2470-1343 |
DOI | 10.1021/acsomega.2c02442 |
Database | MEDical Literature Analysis and Retrieval System OnLINE |
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