Potential Oil and Gas-Bearing Basins of the Qinghai-Tibetan Plateau, China
Chengshan Wang, Edmund Z. Chang, Shaonan Zhang
Abstract
Chengshan Wang, Edmund Z. Chang, Shaonan Zhang
Abstract
A number of composite sedimentary basins are present on the Qinghai-Tibet (Tibetan) Plateau. Some of these basins are filled with marine sediments, whereas others are fault-bounded continental depressions. Mixed source-rock types are present, of variable organic matter content; source rocks are mainly carbonates and secondarily mudstones. Vitrinite reflectance and biomarker analyses show that Mesozoic and Cenozoic source rocks have reached the peak stages of oil generation; older source rocks may have generated natural gas. The hydrocarbon reserves of these basins are believed to total ∼37.2 billion barrels. The Qiangtang-Qamdo basin probably has the greatest potential for oil exploration.
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A number of composite sedimentary basins are present on the Qinghai-Tibet (Tibetan) Plateau. Some of these basins are filled with marine sediments, whereas others are fault-bounded continental depressions. Mixed source-rock types are present, of variable organic matter content; source rocks are mainly carbonates and secondarily mudstones. Vitrinite reflectance and biomarker analyses show that Mesozoic and Cenozoic source rocks have reached the peak stages of oil generation; older source rocks may have generated natural gas. The hydrocarbon reserves of these basins are believed to total ∼37.2 billion barrels. The Qiangtang-Qamdo basin probably has the greatest potential for oil exploration.
Key concepts: Source rock, Geology, Plateau (mathematics), Structural basin, Sedimentary basin, Cenozoic, Geochemistry, Maturity (psychological)