滨里海盆地东缘盐构造及变形机制:物理模拟的启示
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本文为中国石油股份公司项目(编号20016E- 1606)资助的成果。


Salt structure characteristics and deformation mechanism in the eastern margin of Pre- Caspian basin:the implication of physical simulation
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    摘要:

    盐构造与油气成藏关系密切,一直是构造地质和石油地质研究的热点。滨里海盆地下二叠统孔谷阶发育巨厚盐层,并发育盐底辟、盐枕、盐滚、盐边凹陷、盐焊接和龟背等多种盐构造,盐构造类型多、变形机理各异。由于盐构造成因复杂,导致对盐构造宏观变形动力机制、下伏地层微地貌对上覆盐层构造变形影响等认识不清,制约了对盐构造形成机理的认识。本文根据滨里海盆地东缘地震资料和地层特征,建立了地质模型,设计了相应的盐构造物理模拟实验;通过物理模拟实验研究了盐构造变形动态过程,梳理了盐构造变形机理及与下伏地层之间的关系。结果表明:①早期盐层变形动力主要为外部挤压力和盐层滑脱流动变形,滨里海盆地构造变形外力主要来自东部乌拉尔造山作用,造山运动造成盐层塑性流动滑脱变形形成层间褶皱及与盐层相关的断裂;②晚期盐构造幅度和巨厚盐丘形成动力主要为上覆沉积物的差异负载和下伏地层微地貌古构造背景,在滨里海盆地晚二叠世到三叠纪,来自东部乌拉尔褶皱带的碎屑物持续向盆地充填沉积形成差异负载,造成盐层纵向的剧烈变形,而下伏地层正向微地貌加速了这种变形。这些试验结果对滨里海盆地盐相关构造的认识和油气勘探有重要的指导作用。

    Abstract:

    Salt structure is a focus issue of tectonics and petroleum geology research, and is closely related to hydrocarbon accumulation. Thick salt layers are here in Kungurian Formation of the Lower Permian in the Pre- Caspian Basin, and salt- related structures here include salt diapir, salt pillow, salt roller, salt margin depression, salt weld and turtle structure, thus the deformation mechanism is very complicated. However, since the main control factors and dynamic mechanism of the macroscopic deformation of the salt structure, and the influence of the underlying stratum micro- geomorphology on the structural deformation of the overlying salt layers are unclear, insights of the salt structures on hydrocarbon accumulation is restricted. Based on the seismic data of the eastern margin of the Pre- Caspian Basin and the distribution characteristics of the strata, the stratigraphic geological model of the eastern margin of the basin is established, and the physical simulation experiment models are designed accordingly. By physical simulation experiments, the process of salt structure deformation is studied, and the relationship between salt structure deformation mechanism and underlying stratum geomorphology is concluded. Via the construction of physical simulation experiments, industrial CT dynamic monitoring andscanning, and three- dimensional reconstruction techniques, the visualization and dynamization of the research process are realized. Results show that:①〖BP(〗=1\*GB3〖BP)〗The main driving force for the formation of salt structure is the compressive; The structural deformation force of the Pre- Caspian Basin mainly comes from the eastern Ural orogeny; In addition, the detachment of the salt layer will also affect the deformation of the strata, forming inter- layer folds and causing faultsbetween and above salt layers.②〖BP(〗=2\*GB3〖BP)〗From the Late Permian to the Triassic, the uneven deposition of debriscaused bythe differential load to the basin from the Ural fold belt in the eastern part of the Pre- Caspian Basin is also a main driving force for formation of fault structure.These insights have guidingresearch on salt- related structures and oil and gas exploration in the Pre- Caspian Basin.

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景紫岩,李国斌,张亚军,王荣华,谢天峰,崔键,刘文强,代寒松.2021.滨里海盆地东缘盐构造及变形机制:物理模拟的启示[J].地质学报,95(5):1459-1468.
Jing Ziyan, Li Guobin, Zhang Yajun, Wang Ronghua, Xie Tianfeng, Cui Jian, Liu Wenqiang, Dai Hansong.2021. Salt structure characteristics and deformation mechanism in the eastern margin of Pre- Caspian basin:the implication of physical simulation[J]. Acta Geologica Sinica,95(5):1459-1468.

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  • 收稿日期:2020-07-01
  • 最后修改日期:2020-12-11
  • 录用日期:2020-08-27
  • 在线发布日期: 2021-03-30
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