Study on the Provenance and Tectonic Setting of Mudstone in the Lower Silurian Longmaxi Formation of the Yanyuan Basin on the Western Margin of the Yangtze Platform

• Published in: Minerals (Basel) 2023-01, Vol.13 (2), p.194
• Main Authors: Zhang, Qian, Zhang, Bin, Yu, Qian, Men, Yupeng, Zhang, Haiquan, Kang, Jianwei, Cao, Junfeng, Zhao, Ankun, Zhou, Yexin, Feng, Xintao
• Format: Article
• Language: English
• Subjects: Basins (Geology); Continental crust; Continental margins; Discovery and exploration; element geochemistry; Geology; Igneous rocks; Island arcs; Lithology; Longmaxi Formation; Mudstone; Natural gas exploration; Oceanic crust; Oceanic islands; Oil and gas exploration; Platforms (geology); provenance; Quartz; Rocks, Igneous; Sedimentary basins; Sedimentary rocks; Sediments; Sediments (Geology); Shale; Shale gas; Shale oils; Shales; Silurian; tectonic setting; Tectonics; Tectonics (Geology); Yanyuan Basin
• ISSN: 2075-163X; 2075-163X
• DOI: 10.3390/min13020194

This study investigates the provenance and tectonic background of the lower Silurian Longmaxi Formation black shale of the Yanyuan Basin in the western Kangdian ancient land and provides guidance for shale gas exploration and development in the area. The mineral petrological and geochemical characteristics of the Longmaxi Formation black shale in this area have been studied in detail. The study area is mainly a passive continental margin environment, but also has the attributes of an active continental margin and island arc environment due to the collision between the western oceanic crust and the Yangtze continental crust. The source rocks are mainly felsic igneous rocks, with a small contribution of intermediate–basic rocks. It is inferred that the Kangdian ancient land in the eastern part of the area could be the main provenance area, but with the contribution of sediments derived from oceanic island arc located in the west. During the whole Longmaxi period, the tectonic movement was intense, the climate was cold, the degree of chemical weathering was low, and it was a highly volatile geological sedimentary basin. Therefore, the highly siliceous organic-rich mudstone, which was different from the Sichuan Basin, was deposited.