Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (1): 131-138.doi: 10.13278/j.cnki.jjuese.20180129

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Sedimentary Model of Mesozoic in the Southern Part of the East China Sea Shelf Basin

Wang Jiao1,2, Li Zhigao3, Cai Laixing1,2, Gong Qiyong1,2   

  1. 1. Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, Shandong, China;
    2. Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266071, Shandong, China;
    3. Shenzhen Branch, Cnooc(China) co., LTD. Shenzhen 518000, Guangdong, China
  • Received:2018-05-24 Published:2019-01-18
  • Supported by:
    Supported by National Natural Science Foundation of China (41476053),National Marine Geology Special Project of China (DD20160147) and Project of China Geological Survey (DD20160153,DD20190211)

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Abstract: Based on the comprehensive study of sedimentary facies, the authors clarified the sedimentary characteristics of Mesozoic in the southern part of the East China Sea Shelf basin by means of seismic facies analysis. After the unit analysis of paleo-geographic setting,the sedimentary model of Jurassic and Cretaceous in this area is established. In Jurassic, neither Yandang low uplift nor Oujiang pit was formed, and the Minjiang pit and the Keelung pit were integrated. During the Late Cretaceous-Paleocene, with the increase of the subduction angle of the Pacific plate, the Zhejiang-Fujian uplift area was destroyed, forming the Yandang low uplift, and a continental alluvial fan fluvial River delta lake depositional system was deposited in the Oujiang pit in western China. Because the Taipei low uplift had not yet played the role of segmentation, the Minjiang pit in the East and the Keelung pit were still connected, the source came from the Zhejiang-Fujian uplift zone and the Taipei underwater volcanic rock zone. The coastal shallow sea depositional system was developed, and the volcanism had a strong influence.

Key words: East China Sea Shelf basin, Mesozoic, depositional system, sedimentary model

CLC Number: 

  • P618.13
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