1 Key Laboratory of Orogenic Belts and Crustal Evolution,Ministry of Education,School of Earth and Space Sciences, Peking University,Beijing 100871, China; 2 Department of Xinjiang Exploration Project Management,Sinopec Shengli Oilfield Company,Shandong Dongying 257015, China
Abstract：The depositional age,sedimentary environment and tectonic setting of the Permian Lucaogou Formation in eastern Tianshan Mountains are controversial. Based on the standard fossil assemblages of Turfania taoshuyuanensis and Tomiella found in the Lucaogou Formation,the large number of detrital zircons from the sedimentary strata with the youngest peak age of 261 Ma,it is believed that the deposition age of the Lucaogou Formation is Guadalupan(Middle Permian) rather than Uralian(Early Permian). Based on the discovery of typical marine indicator mineral glauconite,the discovery of marine facies or the interactional facies of Tomiella and the confirmation of ultra-high salinity saline lake basin,it is considered that the Lucaogou Formation was mainly lacustrine sediments,but some sedimentary periods were affected by transgression(flooding)events. In eastern Tianshan Mountains,the Permian Lucaogou Formaition of Junggar Basin,Santanghu Basin and Tu-Ha Basins has similar rock assemblages,faunal features and tectonic characteristics,but there are differences in paleo-salinity,paleo-water depth,paleo-climate,paleo-redox conditions and primary productivity among different basins,suggesting that the Lucaogou Formation was deposited in a series of dispersed rift basins,and there is no unified depositional center among different basins.
JIAO Yue,WU Chaodong,WANG Jialin et al. Comparative study on sedimentary characteristics and palaeoenvironment of the Permian Lucaogou Formation in eastern Tianshan Mountains[J]. JOPC, 2023, 25(2): 277-293.
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