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| Sedimentary distribution of evaporites in Wusongge'er Formation in central Tarim Basin and reconstruction of prototype basin |
| Qing Biana,*, JiBiao Zhanga,b,c, Fan Fengb, Yang Lic, ChenJun Huanga, TieYi Wangb, KangKang Guoc |
aPetroleum Exploration and Production Research Institute, Sinopec, Beijing, 100083, China; bNational Energy Laboratory of Carbonate Oil and Gas, Sinopec, Beijing, 100083, China; cKey Laboratory of Deep Geology and Resources, Sinopec, Beijing, 100083, China |
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Abstract The MiddleLower Cambrian Wusongge'er Formation in the Tarim Basin hosts extensive evaporite deposits, yet the formative processes of these evaporites under equatorial arid climates and their tectonosedimentary implications remain poorly constrained. Previous studies, limited to lowresolution seismic data and outcrops in the northwestern margin, failed to resolve depositional variations in the central basin. This study aims to decipher the genetic mechanisms of evaporite precipitation and reconstruct the prototype basin’s tectonosedimentary evolution by integrating highquality 3D seismic data (2023), geophysical forward modeling, and palaeogeographic reconstructions. Integrated analyses revealed a distinct zoned “west haliteeast gypsum/dolomite” pattern driven by paleosalinity gradients in a semiclosed lagoon system, alongside an elongated reef body in the middle ramp and thrombolite buildups in the inner ramp. Evaporite distribution was dominantly controlled by equatorial aridity (climate) and faultinduced differential subsidence (tectonics), with the latter creating thickness variations exceeding 300 m. This study establishes a genetic model of evaporite sedimentation under the Cambrian greenhouse conditions, providing analogues for coeval evaporite systems in Gondwana. The restored prototype basin configuration reveals saltdriven sediment partitioning processes, offering new insights into the tectonosedimentary evolution of intracratonic basins. While seismic interpretations face limitations in deep zones with scarce drilling data, this framework guides future ultradeep exploration targeting salttectonized traps below 8,000 m depth.
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Received: 08 January 2024
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Corresponding Authors:
*Email address: bianqing.syky@sinopec.com (Q. Bian).
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