Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (2): 507-517.doi: 10.13278/j.cnki.jjuese.201502114

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Sandstone Distribution Characteristics and Dispersal Mechanism of the Lower Cretaceous Nantun Formation,Tanan Depression

Yan Lei1, Liu Zhaojun2, Fang Shi2, Zhang Ge3, Zhang Junlong3, Hu Fei2   

  1. 1. Research Institute of Petroleum Exploration & Dvelopment, Petro China, Beijing 100083, China;
    2. College of Earth Sciences, Jilin University, Changchun 130061, China;
    3. Exploration and Development Research Institute, Daqing Oilfield Company Ltd. Daqing 163712, Heilongjiang, China
  • Received:2014-06-03 Published:2015-03-26

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Abstract:

The source direction and sand distribution characteristics of Nantun Formation are concluded by heavy mineral analysis, isopach maps of sandstone and seismic reflection in Tanan depression. The study result shows that the fault system played a role in scattering and blocking of the sediments. According to the relationship between the fault assemble and sandstone distribution characteristics, the fault assemble can be divided into three types, "tilting ladder type", "non-tilting ladder type", and "polar type". Based on the source and sand distribution characteristics, the fault assemble can be divided into "horizontal sand type" and "vertical sand type". To integrate the fault assemble control effect on sand distribution, the two models of sand control mechanism can be concluded, "induced model" and "contained model". This study provides a typical example for the research on the structurally controlled deposition and sand disperse machanism in a rift basin.

Key words: Tanan depression, Nantun Formation, sandstone distribution characteristics, sand-control fracture, dispersal mechanism, sandstone

CLC Number: 

  • P544.4

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