Sedimentological and geochemical characteristics of lower Cambrian Qiongzhusi shale in the Sichuan Basin and its periphery, SW China:Implications for differences in organic matter enrichment  

作　　者：Cheng-Lin Ye Jun-Jun Shen Shan-Shan Li Yu-Man Wang Guang-Chao Tan Jia-Kai Yan Lin Zhou Ji-Yong Liu 

机构地区：[1]Hubei Cooperative Innovation Center of Unconventional Oil and Gas of Yangtze University,Wuhan,430100,Hubei,China [2]College of Geophysics and Petroleum Resources,Yangtze University,Wuhan,430100,Hubei,China [3]Hydrogeology and Engineering Geology Institute of Hubei Geological Bureau,Jingzhou,434020,Hubei,China [4]PetroChina Research Institute of Petroleum Exploration and Development,Beijing,100083,China [5]Exploration and Production Research Institute,Jianghan Oilfield Company,SINOPEC,Wuhan,430100,Hubei,China

出　　处：《Petroleum Science》2024年第6期3774-3789,共16页石油科学(英文版)

基　　金：supported by the Hubei Province Natural Science Geological Innovation Development Joint Funding Project (2024AFD388)。

摘　　要：Few studies have systematically investigated the factors controlling organic matter enrichment in shales from the Qiongzhusi Formation, within and surrounding the Sichuan Basin, under different depositional environments. This has resulted in different academic understandings and limited clarity on the mechanisms of organic matter enrichment. On this premise, in this study, the basic geological characteristics and depositional paleoenvironments of shales along the passive continental margin, the western Hubei Trough, and the western Sichuan Trough were compared and analyzed using core, outcrop, and mineral testing. Furthermore, data from organic geochemical and elemental analyses were utilized to investigate the different enrichment mechanisms and formation modes of the organic matter in different periods. The results reveal that the organic matter enrichment in this region should be mainly influenced by the preservation conditions, paleo-productivity, and terrigenous input. However, there were clear differences in the main controlling factors in the different periods. In the Q1 phase, the region had a high sea level, had the strongest rifting, had the largest accommodation space, and exhibited characteristics of low terrestrial input and bottom water hypoxia. The changes in the paleo-productivity caused by upwelling currents were the main factors controlling the variations in the organic matter enrichment. In the Q2 phase, the weakened decreasing sea level co-occurred with a reduction in the accommodation space across the region. The organic matter enrichment was significantly controlled by the paleo-productivity, preservation conditions, and terrigenous inputs, and the organic matter enrichment conditions deteriorated from the passive continental margin to the western Hubei Trough and western Sichuan Trough. The total organic carbon(TOC) content of the shale decreased significantly. In the Q3 phase, the entire region entered an infilling stage, which was dominated by an oxygen-rich environment,and the preservati

关 键 词：Middle and upper Yangtze region Black shale Organic matter Upwelling currents Depositional paleoenvironment Factors controlling enrichment 

分 类 号：P618.13[天文地球—矿床学]