Citation: | CUI Min, TANG Liang-jie, WANG Peng-hao, GUO Tong-lou, LU Xing-bin. CHARACTERISTICS OF THE PALEO-STRESS IN THE SOUTHWESTERN MARGIN OF XUEFENG UPLIFT AND ITS SIGNIFICANCE FOR PETROLEUM GEOLOGY[J]. Journal of Geomechanics, 2009, 15(3): 289-295. |
Based on the geological survey, balanced cross-section analysis and regional tectonic evolution, we take advantage of rock acoustic emission information to restore the maximum paleo-stress in the southwest margin of Xuefeng Uplift, and discuss the relationship between the maximum paleo-stress and hydrocarbon accumulation and damage. The results show that the study area has undergone five key structural reforms of different intensities. In the early Paleozoic and Indosinian cycle, the tectonic movement is weak, and the maximum paleo-stress are 13.3 MPa and 24 MPa respectively, equivalent to the main accumulation period of Majiang ancient reservoir. The high-frequency and high-intensity paleostress correspond to accumulation and damage of Majiang ancient reservoir. The Neopaleozoic structural deformation with the maximum paleo-stress of 92.6 MPa represents the formation of the reservoir. The Yanshan and Himalayan structural movements, with the restored paleo-stress from 23.3 MPa to 74.4 MPa, cover the period of extensive destruction of paleo-reservoir.
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Distribution of paleo reservoirs around the southwest margin of Xuefeng Uplift
The model for formation and destruction of the Majiang ancient reservoir