Present in situ stress measurement in the eastern segment of Yarlung Zangbo River fault and fault activity analysis

被引:0
|
作者
Sun Wei-feng [1 ]
Huang Huo-lin [2 ]
Sun Dong-sheng [1 ]
Meng Wen [1 ]
Chen Qun-ce [1 ]
机构
[1] Chinese Acad Geol Sci, Inst Geomech, Technol Innovat Ctr In Situ Stress, Minist Nat Resources, Beijing 100081, Peoples R China
[2] PowerChina Huadong Engn Corp Ltd, Hangzhou 311122, Zhejiang, Peoples R China
关键词
in situ stress; hydraulic fracturing method; fault activity; Yarlung Zangbo River fault; Qinghai-Tibet plateau; HYDRAULIC FRACTURING STRESS; QINGHAI-TIBET PLATEAU; TECTONIC STRESS; REGION; STATE; FIELD; EARTHQUAKES; MAGNITUDE; RESERVOIR; BUILDUP;
D O I
10.16285/j.rsm.2023.0545
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
In order to determine the in situ stress state of the newly built hydropower station project in Jiacha county, and understand the activity of the eastern segment of the Yarlung Zangbo River fault zone, we obtained the in situ stress data in the engineering field by using the self-developed deep-hole stress measuring equipment based on the hydraulic fracturing method. We analyzed the fault activity by employing the Mohr-Coulomb failure criterion and the collected in situ stress data along the eastern segment of the Yarlung Zangbo River fault zone. The results showed that: (1) The magnitudes of the maximum horizontal stress SH ranged from 6.07 MPa to 37.62 MPa, the values of the minimum horizontal stress Sh were from 3.13 MPa to 20.33 MPa at the depth from 122.75 m to 418.75 m, and the dominant direction of the measured maximum horizontal principal stress was nearly NNE. (2) The stress regime was mainly characterized by SH> Sh> Sv (Sv is the vertical principal stress), which was prone to reverse faulting. (3) Most of the measured and collected Mohr stress circles intersected the failure threshold line with friction coefficient equal to 0.6, which indicated that the eastern segment of the Yarlung Zangbo River fault zone was in a high level of fault slip instability. Furthermore, the fault slip risk of the west section from Gongga to Langxian was higher than that of the east section near Linzhi along the eastern segment of the Yarlung Zangbo River fault zone.
引用
收藏
页码:1129 / 1141
页数:13
相关论文
共 70 条
  • [1] Focal depths and mechanisms of shallow earthquakes in the Himalayan-Tibetan region
    Bai, Ling
    Li, Guohui
    Khan, Nangyal G.
    Zhao, Junmeng
    Ding, Lin
    [J]. GONDWANA RESEARCH, 2017, 41 : 390 - 399
  • [2] State of Tectonic Stress in Northeast India and Adjoining South Asia Region: An Appraisal
    Baruah, Santanu
    Baruah, Saurabh
    Kayal, J. R.
    [J]. BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2013, 103 (2A) : 894 - 910
  • [3] [卞爽 Bian Shuang], 2021, [地质力学学报, Journal of Geomechanics], V27, P178
  • [4] Estimating the Least Principal Stress in a Granitic Rock Mass: Systematic Mini-Frac Tests and Elaborated Pressure Transient Analysis
    Broeker, Kai
    Ma, Xiaodong
    [J]. ROCK MECHANICS AND ROCK ENGINEERING, 2022, 55 (04) : 1931 - 1954
  • [5] FRICTION OF ROCKS
    BYERLEE, J
    [J]. PURE AND APPLIED GEOPHYSICS, 1978, 116 (4-5) : 615 - 626
  • [6] [曹忠权 Cao Zhongquan], 2003, [地球物理学进展, Progress in Geophysiscs], V18, P167
  • [7] Chen P., 2023, Rev. Geophys. Planet. Phys., V54, P667
  • [8] [陈群策 Chen Qunce], 2019, [地质力学学报, Journal of Geomechanics], V25, P853
  • [9] [陈群策 Chen Qunce], 2010, [地球学报, Acta Geoscientia Sinica], V31, P541
  • [10] Chen ZHANG, 2022, Journal of Seismological Research, V45, P526