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Volume 29 Issue 2
Mar 2018
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Dan Gao, Rihui Cheng, Yanjie Shen, Liaoliang Wang, Xiaoqiang Hu. Weathered and Volcanic Provenance-Sedimentary System and Its Influence on Reservoir Quality in the East of the Eastern Depression, the North Yellow Sea Basin. Journal of Earth Science, 2018, 29(2): 353-368. doi: 10.1007/s12583-017-0945-z
Citation: Dan Gao, Rihui Cheng, Yanjie Shen, Liaoliang Wang, Xiaoqiang Hu. Weathered and Volcanic Provenance-Sedimentary System and Its Influence on Reservoir Quality in the East of the Eastern Depression, the North Yellow Sea Basin. Journal of Earth Science, 2018, 29(2): 353-368. doi: 10.1007/s12583-017-0945-z

Weathered and Volcanic Provenance-Sedimentary System and Its Influence on Reservoir Quality in the East of the Eastern Depression, the North Yellow Sea Basin

doi: 10.1007/s12583-017-0945-z
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  • Corresponding author: Rihui Cheng, chengrh@jlu.edu.cn
  • Received Date: 15 Feb 2017
  • Accepted Date: 20 Aug 2017
  • Publish Date: 01 Feb 2018
  • Seismic stratigraphy, core logging and the data from cores are used to identify the development and evolution of the east provenance-sedimentary system and to analyze its influence on the quality of reservoirs in the eastern depression of the North Yellow Sea Basin. The eastern provenance-sedimentary system is a fan delta (delta) and subaqueous fan sedimentary system with volcanic provenance. Its evolution is closely related to internal uplift and coeval volcanic activity. During faulting and volcanic activity, an internal uplift gradually formed and the eastern provenance-sedimentary system began to develop. Clastic materials from the weathered uplift and volcanic activity were the main sources of sediment and were deposited in the Middle Jurassic to the Early Cretaceous. A subaqueous fan sedimentary system developed in the Middle Jurassic, a deltaic to subaqueous fan sedimentary system developed in the Late Jurassic, and a fan delta to subaqueous fan sedimentary system developed in the Early Cretaceous. The volcaniclastic detritus was mainly composed of acidic materials with a small amount of intermediate materials. The reservoir in the eastern sedimentary system is a type of tight sandstone with ultra-low porosity and very low permeability due to the influence of volcanism and diagenesis. The reservoir quality is worse than those of the northern and the western sedimentary systems. However, the high volume of volcanic materials and deep-marine sedimentary conditions resulted in good-quality hydrocarbon source rocks that ensures the exploration potential in the eastern sedimentary system reservoir.

     

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