Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (1): 18-30.doi: 10.13278/j.cnki.jjuese.20190002

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Establishment of Stratigraphic Framework of Late Permian to Early Triassic in Northern Jiangsu and South Yellow Sea Basin Based on Land-Sea Comparison

Li Wenqiang1,2,3, Guo Xingwei2,3, Wang Yanzhong1,3, Cai Laixing2,3, Zhang Xunhua3,4, Wu Zhiqiang2,3, Yang Tian1,3, Gao Xiaohui2,3, Zhao Dongdong5   

  1. 1. School of Geosciences, China University of Petroleum, Qingdao 266580, Shandong, China;
    2. Qingdao Institute of Marine Geology, Qingdao 266071, Shandong, China;
    3. Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266071, Shandong, China;
    4. Nanjing Center, China Geological Survey, Nanjing 210016, China;
    5. Shandong Bureau of China Metallurgical Geology Bureau, Qingdao 266109, Shandong, China
  • Received:2019-01-03 Published:2020-02-11
  • Supported by:
    Supported by National Marine Geology Special Program of China (DD20160147) and National Natural Science Foundation of China (41776081)

Abstract: We studied the sedimentary strata and identified the sequential interfaces of the northern Jiangsu and South Yellow Sea basin by using lithology, well logging, paleontology and other data, and divided the Upper Permian-Lower Triassic strata of the research area into two large cycles (LC1 and LC2) and three intermediate cycles (MC1-MC3) based on continental shelf drilling program Well CSDP-2, in combination with Well N5, Well WX5-ST1 and typical section of Jiangning area in Nanjing under the theoretical instruction of sequence stratigraphy and sedimentology. This research shows that the South Yellow Sea basin and the northern Jiangsu basin are actually the same sedimentary basin separated by coastlines, and their Upper Permian-Lower Triassic strata are very well comparable. The LC1 large scale cycle has obvious asymmetry, and the highest base level MFS1 corresponds to the mudstone of shallow sea shelf facies in the middle and lower part of Longtan Formation. The LC2 large scale cycle was denuded by the Indosinian movement, and only half cycle of the basic-level rising remains. The study area mainly developed tidal flat, lagoon, delta and other marine and land transitional facies in the MC1 cycle (Longtan Formation), indicating the relatively stable water depth from place to place; however, during the MC2 and MC3 cycles (Dalong Formation and Qinglong Formation), the sedimentary facies such as shallow sea shelf, tidal flat, lagoon,and carbonate platform developed, and the water became deeper in the southwest and shallower in the northeast. This is the result of basin differential uplifts during Tungwu Movement.

Key words: land-ocean comparison, Late Permian to Early Triassic, stratigraphic framework, the northern Jiangsu and South Yellow Sea basin, Well CSDP-2

CLC Number: 

  • P618.13
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