| Citation: | DENG Kong，LU Yangbo，ZHANG Bolin，et al. Controls of Middle and Late Permian major geological events on the development of the organic-rich shales in northeast Sichuan Basin[J]. Bulletin of Geological Science and Technology，2025，44（2）：1-21 doi: 10.19509/j.cnki.dzkq.tb20240483
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Three sets of black organic-rich shales found in the Permian Dalong Formation, Wujiaping Formation, and Maokou Formation in northeastern Sichuan have yielded significant discoveries in shale gas exploration, presenting new opportunities beyond the established Wufeng-Longmaxi marine shale gas plays.
This study investigated the lithological characteristics and paleoenvironmental evolution of these formations through petrological and geochemical analyses. A comprehensive examination of the depositional environments and the key controlling factors for organic matter enrichment during the deposition of these organic-rich black shales from the Middle to Late Permian in northeastern Sichuan has been performed.
The findings demonstrate that the three organic-rich shales exhibit considerable heterogeneity, with distinct controlling factors influencing their development. The sedimentary period of the third member of the Maomao Formation was characterized by strong upwelling, weak volcanic activity, and limited hydrothermal activities. This environment featured a warm and humid climate, extremely high primary productivity, low terrestrial input, and anoxic sulfide water conditions. In contrast, the sedimentary environment of the second member of the Wujiaping Formation was marked by high productivity, low continental source input, seasonal upwelling, weak hydrothermal activity, and interstitial sulfidation-sulfidation conditions and driven by strong hydrothermal fluid, upwelling, and island arc volcanic activity. The sedimentary environment of the Dalong Formation also exhibited high primary productivity, low terrestrial input, and interstitial sulfidation-sulfidation conditions.
The research highlights the complex interactions of multiple geological events on organic-rich shales and constructs a genetic model for these shales influenced by various geological factors. This model provides a theoretical basis and supports the identification of favorable areas for marine shale gas exploration.
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