A Seismic Evidence for the Reliability of the 3-D Stress Measurement by Hydraulic Fracturing

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Determining the in-situ stress of wall rock is important for the underground cavern project. The three-dimensional (3-D) stress measurement, which is obtained by hydraulic fracturing stress measurement via measuring the stresses in boreholes with three different orientations, has been applied for the designation of cavern project. However, there are few examples that can demonstrate the reliability of 3-D stress measurement method. In this study, we showed one example of the 3-D stress results measured by hydraulic fracturing in Western China. The measured results, especially the dip angles of the maximum principle stress are consistent with those determined by focal mechanism of nearby earthquakes. This consistence indicates the reliability of the 3-D stress results by hydraulic fracturing and an expected application for regional geostress study.

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307-311

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January 2014

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© 2014 Trans Tech Publications Ltd. All Rights Reserved

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[1] B. C. Haimson, A Comparitive of Deep Hydrofracturing and Overcoring Sress Measurements at Six Locations With Particular Interest to the Nevada Test Site, Hydraulic Fracturing Stress Measurements, National Academy Press (1983).

Google Scholar

[2] F. Rummel, Hydraulic Fracturing Stress Measurement along the Eastern Boundary of the SW-German Block, Hydraulic Fracturing Stress Measurements, National Academy Press (1983).

Google Scholar

[3] H. Tsukahara, R. Ikeda, Tectonophys, (1986), 135(4), 329~345.

Google Scholar

[4] M. K. Hubert, D. G. Willis, Mechanics of hydraulic fracturing, Mem. Amer. Assoc. Petrol. Geol., (1957), 18, 239~257.

Google Scholar

[5] C. Fairhurst, Rock Mech., (1964), 2, 129~147.

Google Scholar

[6] M. Cai, The principle and technique of stress measurement (revised edition, in Chinese), Science Press, Beijing (2000).

Google Scholar

[7] Y. Mizuta, O. Sano, S. Ogino and H. Katoh, Int. J. Rock Mech Min Sci & Geomech Abstr. (1987), 24(1), 15~29.

Google Scholar

[8] M. Kuriyagawa, H. Kobayashi, I. Matsunaga, T. Yamaguchi and K. Hibiya, Int. J. Rock Mech Min Sci & Geomech. Abst., (1989), 26(6), 587~593.

Google Scholar

[9] Q. Guo, L. Bao, L. Ding and J. Xu, The application of the 3-D hydraulic fracturing stress measurement in the deep underground cavern project, 46th U. S. Rock Mechanics/Geomechanics Symposium, June 24-27, Chicago, IIIinois, (2012).

Google Scholar

[10] Q. Guo, S. Zhao, L. Ding and C. Wang, Chinese J. Rock Mech. & Eng, (2007), 26(supp. 1), 3361~3366.

Google Scholar

[11] M. Wu, Y. Zhang, C. Liao, Q. Chen, Y. Ma, J. Wu, J. Yan and M. Ou, Acta Geologica Sinica, (2010), 84(9), 1292~1299.

Google Scholar

[12] Y. Chen, Z. Yang, Y. Zhang and C. Liu, Science in China: Earth Science, (2013), 43(6), 1064~1072.

Google Scholar

[13] X. Hu, C. Yu, K. Tao, X. Cui, J. Ning and Y. Wang, Chinese J. Geophys. (in Chinese), (2008), 51(6), 1711~1788.

Google Scholar

[14] J. Lü, X. Wang, J. Su, L. Pan, Z. Li, L. Yin, X. Zeng and H. Deng, Chinese J. Geophys. (in Chinese), (2013), 56(5), 1753~1763.

Google Scholar

[15] Information on http: /www. cea. gov. cn.

Google Scholar

[16] Q. Guo, C. Wang, H. Ma and C. Wang, Chinese J. Geophys. (in Chinsese), (2009), 52(5), 1395~1401.

Google Scholar