Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (1): 39-52.doi: 10.13278/j.cnki.jjuese.20180113

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Characteristics of Lower Silurian Hydrocarbon Source Rocks and Their Main Controlling Factors in the South Yellow Sea Basin Based on Land-Ocean Comparison in the Lower Yangtze Region

Cai Laixing1,2, Xiao Guolin1,2, Guo Xingwei1,2, Wang Jiao1,2, Wu Zhiqiang1,2, Li Baogang3   

  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. School of Geosciences, China University of Petroleum(East China), Qingdao 266580, Shandong, China
  • Received:2018-09-07 Published:2019-01-18
  • Supported by:
    Supported by National Marine Geology Special Project of China (DD20160147), National Natural Science Foundation of China (41210005, 41776081) and Applied Basic Research Program of Qingdao (2016239)

Abstract: To meet the demand of marine origin oil-gas exploration in the South Yellow Sea basin, the authors systematically analyzed and compared the palaeo-geographic setting and sedimentary filling characteristics of Early Silurian between the South Yellow Sea basin and the land area in the Lower Yangtze plate based on the geological data of Jiangsu, Zhejiang, Anhui regions and the cores of well-2,then summarized the characteristics of the Lower Silurian hydrocarbon source rocks,and further discussed their main controlling factors in the South Yellow Sea basin. The results showed that two sets of source rocks of the Fentou Formation and the upper part of the Gaojiabian Formation were drilled in the well CSDP-2, which are thick, dark and silty mudstone with low abundance type Ⅱ2 organic matter, and all of them are at over-maturity stage. Controlled by the development stage of global transgression and the tectonic activity of the Yangtze plate, the Early Silurian sedimentary environment in the lower Yangtze region gradually changed from initial deep water shelf to shallow water shelf. In addition, under the influence of the early high primary productivity and good preservation condition, the source rock quality in the lower part of the Gaojiabian Formation is obviously better than that in its upper part, and the abundance of organic matter in the black graptolite shale in the bottom section is the highest. Therefore, we believe that there should be a set of high quality hydrocarbon source rocks at the bottom of the Gaojiabian Formation in the South Yellow Sea basin, which can serve as the next key layer for shale gas exploration.

Key words: source rock evaluation, main controlling factors, Lower Silurian, land-ocean comparison, South Yellow Sea basin

CLC Number: 

  • P618.13
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