Lithofacies characteristics and genetic mechanism of hybrid sedimentary rocks in Da'anzhai member, Sichuan Basin
文献类型:期刊论文
| 作者 | Yerejiepu Habulashenmu; Xiaojuan Wang; Longwei Qiu; Yongqiang Yang; Shaoyun Chen; Danish Khan; Jiayi Teng; Yilong Hu |
| 刊名 | Marine and Petroleum Geology
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| 出版日期 | 2024 |
| 卷号 | 162页码:106695 |
| 关键词 | Lithofacies Characteristics Hybrid Sedimentation Genetic Mechanism Da'anzhai Member Sichuan Basin |
| DOI | 10.1016/j.marpetgeo.2024.106695 |
| 英文摘要 | The Jurassic Da'anzhai Member in the Sichuan Basin is a stratigraphic unit characterized by widespread mudstone and hybrid sedimentation. It comprises various lithofacies types and sedimentary structures, including massive structure, laminated structure, mud rip-up clasts and erosion surfaces. By means of detailed analysis of core, logging, thin sections, scanning electron microscope, XRD and XRF data, six lithofacies types are identified in the Da'anzhai Member, and the genetic mechanisms of these lithofacies such as sandy debris flow, turbidity current, bioclastic flow and still water sedimentation are analyzed based on the characteristics of lithofacies. A complete third-order cycle was identified in the LA 1 and RA 1 well based on the variation in the value of gamma ray, bioclastic content as well as lithofacies characteristics. The paleo-sedimentary environment of Da'anzhai Member of Sichuan Basin is reconstructed on the basis of geochemical proxies such as Sr/Cu, Ca/(Ca + Fe), V/(V + Ni), V/Cr, Ti, Al, Al/(Al + Fe) and Fe/Mn. Different sedimentary environments in the Da'anzhai Member controlled the characteristics of lithofacies distribution and the lake level (water depth) primarily controlled the scale and frequency of the development of hybrid sedimentation and mudstone. During the early and late sedimentary periods of the Da'anzhai Member, the climate was arid, water salinity was high, reducing conditions were weak, and the water body was deep. Sediments such as sandy and bioclastic materials in shallow areas were transported to deeper areas through gravity flows under the influence of sudden events like earthquakes, floods or storms and interbedded with still water mudstones. In the middle period of the Da'anzhai Member, the climate was humid, water salinity was low, reducing conditions were strong, and the water body remained deep. A large amount of deep-water mudstone developed in this period, with gravity flow deposits appearing as thin layers. Finally, the comprehensive sedimentary model of the study area is completed based on this characteristics.
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| URL标识 | 查看原文 |
| 语种 | 英语 |
| 源URL | ![]() |
| 专题 | 地球化学研究所_矿床地球化学国家重点实验室 |
| 作者单位 | 1.National Key Laboratory of Deep Oil and Gas, China University of Petroleum (East China), Qingdao 266580, China 2.School of Geosciences, China University of Petroleum, Qingdao 266580, China 3.PetroChina Southwest Oil and Gas Field Company, Chengdu 610041, China 4.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China |
| 推荐引用方式 GB/T 7714 | Yerejiepu Habulashenmu,Xiaojuan Wang,Longwei Qiu,et al. Lithofacies characteristics and genetic mechanism of hybrid sedimentary rocks in Da'anzhai member, Sichuan Basin[J]. Marine and Petroleum Geology,2024,162:106695. |
| APA | Yerejiepu Habulashenmu.,Xiaojuan Wang.,Longwei Qiu.,Yongqiang Yang.,Shaoyun Chen.,...&Yilong Hu.(2024).Lithofacies characteristics and genetic mechanism of hybrid sedimentary rocks in Da'anzhai member, Sichuan Basin.Marine and Petroleum Geology,162,106695. |
| MLA | Yerejiepu Habulashenmu,et al."Lithofacies characteristics and genetic mechanism of hybrid sedimentary rocks in Da'anzhai member, Sichuan Basin".Marine and Petroleum Geology 162(2024):106695. |
入库方式: OAI收割
来源:地球化学研究所
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