Sedimentary evolution of the late Paleozoic in Ordos Basin and its adjacent areas
Li Wen-Hou1, Zhang Qian1, Li Ke-Yong2, Chen Qiang3, Guo Yan-Qin4, Ma Yao4, Feng Juan-Ping2, Zhang Dao-Feng5
1 Department of Geology/State Key Laboratory of Continental Dynamics,Northwest University,Xi'an 710069,China; 2 College of Geology and Environment/Periodical Center,Xi'an University of Science and Technology,Xi'an 710054,China; 3 College of Earth Science and Resources,Chang'an University,Xi'an 710064,China; 4 School of Earth Sciences and Engineering,Xi'an Shiyou University,Shaanxi Key Laboratory of Petroleum Accumulation Geology,Xi'an 710065,China; 5 Research Institute of Exploration and Development,PetroChina Changqing Oilfield Company,Xi'an 710018,China
Abstract：Based on the detailed studies of the late Paleozoic in the Ordos Area for decades,including field measurements,stratigraphy and sequence stratigraphy,geochemistry and geochronology studies,the authors have analyzed lithological characteristics,stratum thickness,stratum contact relationship,sediment provenance and sedimentary facies types. We propose that the Ordos area during the late Paleozoic is a part of the North China Platform. Based on this study,all stages of late Paleozoic sedimentary facies map of the Great Ordos Area was drawn. These maps extended the eastern and southern part of the original Ordos Area,which provided a new evidence for the restoration of the original sedimentary features of the North China Platform in this period.
Li Wen-Hou,Zhang Qian,Li Ke-Yong et al. Sedimentary evolution of the late Paleozoic in Ordos Basin and its adjacent areas[J]. JOPC, 2021, 23(1): 39-52.
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