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    Volume 40 Issue 12
    Dec.  2015
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    Article Navigation >  Earth Science  > 2015  >  40(12): 1987-2001
    Fu Xiaowei, Zhu Weilin, Chen Chunfeng, Zhong Kai, Xu Changhai, 2015. Detrital Zircon Provenance of Upper Mingyuefeng Formation in West Slope of Lishui-Jiaojiang Sag, the East China Sea. Earth Science, 40(12): 1987-2001. doi: 10.3799/dqkx.2015.178
    Citation: Fu Xiaowei, Zhu Weilin, Chen Chunfeng, Zhong Kai, Xu Changhai, 2015. Detrital Zircon Provenance of Upper Mingyuefeng Formation in West Slope of Lishui-Jiaojiang Sag, the East China Sea. Earth Science, 40(12): 1987-2001. doi: 10.3799/dqkx.2015.178
    shu

    Detrital Zircon Provenance of Upper Mingyuefeng Formation in West Slope of Lishui-Jiaojiang Sag, the East China Sea

    doi: 10.3799/dqkx.2015.178
    • 1.

      State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

    • 2.

      China National Offshore Oil Corporation, Beijing 100010, China

    • 3.

      Shanghai Branch of CNOOC Ltd., Shanghai 200030, China

    • Received Date: 2015-06-17
    • Publish Date: 2015-12-15
      Abstract
    • Sedimentary source has a significant impact on the development of oil and gas reservoir. To differentiate the provenance and analyze the lithological composition of the source area of the upper Mingyuefeng Formation in the west slope of Lishui-Jiaojiang sag, 4 detrital zircon samples from 4 drillings were selected for U-Pb isotopic dating, and then provenance analysis was conducted according to the dating results and the age and lithology of potential source. The results suggest that detrital zircons are mainly dominated by magmatic zircons falling into the age ranges of 125-90 Ma, 145-125 Ma and 170-145 Ma, and there are a small amount of metamorphic zircons aged 235-210 Ma and 2 087-1 653 Ma. In the potential source area, volcanic rocks in the age range of 168-94 Ma are in overwhelming majority, and metamorphic rocks older than 210 Ma and intrusive rocks formed in 107.0-87.8 Ma outcrop sporadically, while maybe there are sedimentary rocks of Yongkang Group concentrated locally. The comprehensive analysis shows that the provenance of the northeastern part of the study area was mainly volcanic-sedimentary rocks of Yongkang Group and volcanic of Jiuliping Formation and Late Cretaceous intrusions exposed locally. While in the southwestern part, the source rock was mainly Proterozoic metamorphic rocks and volcanic rocks from Xishantou Formation in addition to Jiuliping Formation, and a small amount of Jurassic volcanic rocks as well., which is more favorable to the development of high-quality reservoir in the southwestern part.

       

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