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    中国百强科技报刊

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    Volume 37 Issue 3
    May  2012
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    Article Contents
    SHI Shuang-shuang, REN Jian-ye, ZHANG Shun, FU Xiu-li, TANG Sheng-min, 2012. Sequence Stratigraphic Framework and Its Formation Mechanism of Post-Rift Inversion Successions in North of Songliao Basin, China. Earth Science, 37(3): 545-555. doi: 10.3799/dqkx.2012.061
    Citation: SHI Shuang-shuang, REN Jian-ye, ZHANG Shun, FU Xiu-li, TANG Sheng-min, 2012. Sequence Stratigraphic Framework and Its Formation Mechanism of Post-Rift Inversion Successions in North of Songliao Basin, China. Earth Science, 37(3): 545-555. doi: 10.3799/dqkx.2012.061

    Sequence Stratigraphic Framework and Its Formation Mechanism of Post-Rift Inversion Successions in North of Songliao Basin, China

    doi: 10.3799/dqkx.2012.061
    • Received Date: 2011-05-28
      Available Online: 2021-11-09
    • Publish Date: 2012-05-01
    • The principle and method of high resolution sequence stratigraphy are employed to deal with seismic reflection profiles, well logs and core data. The sequence stratigraphic framework of post-rift inversion successions has been reconstructed in north of Songliao basin. According to the information of basin fillings, lacustrine level changes and regional tectonic evolution, the geological property and formation mechanism of sequence boundaries are analyzed. The sedimentary filling evolution model is built in post-rift inversion successions. The study indicates that both the 1st-order unconformity SB02 and the 2nd-order ones SB03/SB11 in post-rift inversion successions are responding surfaces to regional compression tectonic events. The styles of systems tracts in the 3rd-order sequences are controlled by lacustrine level changes and provenance supply. The 7 4th-order sequences identified in the second and third members of Nenjiang Formation formed under the conditions of enough provenance and low tectonic subsidence rate during the highstand systems tract of 3rd-order lacustrine level cycle. An important isochronous stratigraphic architecture has been provided for exploration of subtle reservoir in the middle-shallow layers in north of Songliao basin.

       

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