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    Volume 39 Issue 10
    Oct.  2014
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    Article Contents
    Zhang Peng, Feng Chengjun, Sun Weifeng, Yang Haiyu, Tan Chengxuan, 2014. In-Situ Stress Measurement of Deep Borehole in North Segment of Jinzhou Fracture Belt and Analysis on Its Activity. Earth Science, 39(10): 1295-1306. doi: 10.3799/dqkx.2014.122
    Citation: Zhang Peng, Feng Chengjun, Sun Weifeng, Yang Haiyu, Tan Chengxuan, 2014. In-Situ Stress Measurement of Deep Borehole in North Segment of Jinzhou Fracture Belt and Analysis on Its Activity. Earth Science, 39(10): 1295-1306. doi: 10.3799/dqkx.2014.122

    In-Situ Stress Measurement of Deep Borehole in North Segment of Jinzhou Fracture Belt and Analysis on Its Activity

    doi: 10.3799/dqkx.2014.122
    • Received Date: 2014-01-15
    • Publish Date: 2014-10-01
    • Haicheng earthquake occurred in the north segment of Jinzhou fracture belt which is the most important active tectonic structure controlling earthquakes in Liaodong Peninsula. In this study, data was collected from 27 in-situ stress and 5 directional testing sensors installed at varying intervals along the total depth of single 600 m borehole located inside a granite rich region in the north segment of Jinzhou fracture belt at the east part of Xiongyue city. Combined with in-situ stress data of SV > SH > Sh, core sampling of the structural features of shallow earth crust rock formations reveals that the vertical principal stress plays a leading role in normal fault activity. Moreover, measured maximum in-situ principal stress trends towards the northeast-east direction and reflects present tensile properties, with dextral activity, of the Jinzhou segment. The results confirm the previous relevant studies, enriching the dynamics data and facilitating the understanding of the active features of the north segment of the Jinzhou fracture belt.

       

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