Volume 42 Issue 7
Jul.  2017
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Ma Yiquan, Du Xuebin, Liu Huimin, Lu Yongchao, 2017. Characteristics, Depositional Processes, and Evolution of Shale Lithofaceis of the Upper Submember of Es4 in the Dongying Depression. Earth Science, 42(7): 1195-1208. doi: 10.3799/dqkx.2017.097
Citation: Ma Yiquan, Du Xuebin, Liu Huimin, Lu Yongchao, 2017. Characteristics, Depositional Processes, and Evolution of Shale Lithofaceis of the Upper Submember of Es4 in the Dongying Depression. Earth Science, 42(7): 1195-1208. doi: 10.3799/dqkx.2017.097
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Characteristics, Depositional Processes, and Evolution of Shale Lithofaceis of the Upper Submember of Es4 in the Dongying Depression

doi: 10.3799/dqkx.2017.097
  • 1.

    Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China

  • 2.

    Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

  • 3.

    College of Marine Science and Technology, China University of Geosciences, Wuhan 430074, China

  • 4.

    Geological Research Institute of Shengli Oilfield Company, Sinopec, Dongying 257000, China

  • Received Date: 2016-12-07
  • Publish Date: 2017-07-15
    Abstract
  • Organic-rich lacustrine shales have high hydrocarbon potential, but relevant studies did not start until recently, suffering from many deficiencies including relatively few studies on lithofaceis, depositional process and origin and evolution of lacustrine shales. The lacustrine shale succession of the upper submember of Es4 in the Dongying depression, Bohai Bay basin, eastern China, is the most important hydrocarbon source rock and an unconventional reservoir. In this study, we conduct detailed lithofacies characterization to the upper submember of Es4 shale succession in the NY1 drilling core by combining core descriptions, microscopic observations, mineralogy, major and minor elements and log data. Based on the theories of petrography, sedimentology, element geochemistry and T-R sequence stratigraphy, lithofacies features, depositional process of lithofacies, coupling relationship between lithofacies and sequence stratigraphy, and evolutions of paleoclimate and paleolake are investigated in detail. Four major lithofacies associations are identified, including the interbedded evaporite and shale lithofacies association, silt-bearing clay-rich shale lithofacies association, the massive calcareous shale lithofacies association, and the laminated calcareous shale lithofacies association from bottom to top. These lithofacies associations are interpreted to be deposited in small salt lake, a pro-delta environment, shallow lacustrine environment and deep, stratified, anoxic lake, respectively. By contrast, there is coupling between dominant lithofacies and system tracts through time. The changes of dominant lithofacies in the upper submember of Es4 shale succession through time suggest that paleoclimate changed from arid to humid and paleolake changed from small and shallow lake to large and deep lake, and it is inferred that paleolake evolution was controlled by paleoclimate changes and the tectonic subsidence associated with the development of depression-bounding faults.

     

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