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    Volume 42 Issue 11
    Nov.  2017
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    Article Navigation >  Earth Science  > 2017  >  42(11): 1955-1971
    Chen Hehe, Zhu Xiaomin, Huang Handong, Shi Ruisheng, Luo Yaneng, Cui Gang, 2017. Sediment Provenance of Shahejie Formation in Lixian Slope of Raoyang Depression Based on the Detrital Zircon Dating Analysis. Earth Science, 42(11): 1955-1971. doi: 10.3799/dqkx.2017.124
    Citation: Chen Hehe, Zhu Xiaomin, Huang Handong, Shi Ruisheng, Luo Yaneng, Cui Gang, 2017. Sediment Provenance of Shahejie Formation in Lixian Slope of Raoyang Depression Based on the Detrital Zircon Dating Analysis. Earth Science, 42(11): 1955-1971. doi: 10.3799/dqkx.2017.124
    shu

    Sediment Provenance of Shahejie Formation in Lixian Slope of Raoyang Depression Based on the Detrital Zircon Dating Analysis

    doi: 10.3799/dqkx.2017.124
    • 1.

      State Key Laboratory of Petroleum Resource and Prospecting, Beijing 102249, China

    • 2.

      College of Geosciences, China University of Petroleum, Beijing 102249, China

    • 3.

      EOR Research Institute, China University of Petroleum, Beijing 102249, China

    • 4.

      No.1 Oil Production Plant Geological Institute, Huabei Oil Field Branch Company, Renqiu 062552, China

    • Received Date: 2017-05-14
    • Publish Date: 2017-11-15
      Abstract
    • The purpose of this study is to clarify the relationship between sediment provenance combination and sedimentary system of the Member 1 of Paleogene Shahejie Formation, Lixian county slope, Raoyang depression. According to the characteristics of sedimentary gentle slope in Raoyang sag, the distribution of the source systems and "Source-to-Sink" configuration of the Member 1 of Paleogene Shahejie Formation are discussed, based on the detrital zircon U-Pb dating and traditional method of provenance analysis in this study. According to the difference of paleo geomorphology and drilling distribution characteristics, the slope is divided into three areas, A, B and C, which correspond to three provenance systems respectively. More specifically, in terms of the northwest provenance system, the provenance is the Paleozoic igneous rocks from the Xing-Meng orogenic belt, carried by ancient Daqing river system from the northwest to the A district of theslope. As to the west provenance system, the provenance is the Mesozoicigneous rocks, the Meso-Neoproterozoicintrusive rocks, the Mesoproterozoic metamorphic rocks in Laiyuan district, carried by the ancient Tanghe river system from west to the B district of the slope. In the case of the southwest provenance system, the provenance is the Paleoproterozoic metamorphic rocks, carried by the ancient Dasha river system from the southwest to the C district of the slope. There is a positive correlation between detrital zircon content and drainage area.

       

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