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    中国百强科技报刊

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    Volume 44 Issue 8
    Aug.  2019
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    Article Contents
    Zhou Jie, Yang Xibing, Yang Jinhai, Gan Jun, Wu Hao, He Xiaohu, Hu Bin, 2019. Structure-Sedimentary Evolution and Gas Accumulation of Paleogene in Songnan Low Uplift of the Qiongdongnan Basin. Earth Science, 44(8): 2704-2716. doi: 10.3799/dqkx.2019.104
    Citation: Zhou Jie, Yang Xibing, Yang Jinhai, Gan Jun, Wu Hao, He Xiaohu, Hu Bin, 2019. Structure-Sedimentary Evolution and Gas Accumulation of Paleogene in Songnan Low Uplift of the Qiongdongnan Basin. Earth Science, 44(8): 2704-2716. doi: 10.3799/dqkx.2019.104

    Structure-Sedimentary Evolution and Gas Accumulation of Paleogene in Songnan Low Uplift of the Qiongdongnan Basin

    doi: 10.3799/dqkx.2019.104
    • Received Date: 2019-01-21
    • Publish Date: 2019-08-15
    • Based on the detailed interpretation of regional long section and the latest drilling, logging and seismic data, the Paleogene structural pattern, slope type and its evolution characteristics, sedimentary characteristics and their relationship with gas accumulation in Songnan low uplift (SLU)and surrounding areas are analyzed.The purpose is to clarify the tectonic and sedimentary evolution characteristics of the SLU and its influence on gas accumulation. The results show that the SLU is mainly controlled by the No.2 & No.12 faults in the north and No.11 & No.10 faults in the south. The SLU experienced two stages, namely, the differential updip uplift characterized by the "high in the west and low in the east " and the accelerated eastward updip uplift. And it was dominated by the development of rotational lift ramp in the Paleogene. The paleogeomorphology has the characteristics of "alternation of uplift and depression" and "high in the west and low in the east" in study area. The faults activity and uplift of upwarping controlled the distribution of material source area, sedimentary pattern of gentle slope and sand transport channel, so fans delta deposit developed in the gentle slope zone on the western bulge. The wide distribution of fan deltas formed high quality reservoir, and the tectonic activity formed many types of traps. The gas generation, transportation and accumulation are well matched in space and time in the SLU Therefore, the Paleogene of SLU is expected to be the next gas accumulation area of about 100 billion cubic meters in the Qiongnan Basin.

       

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