參考文獻 |
[1] Boness, N. L., and Zoback, M. D., “Stress-induced seismic velocity anisotropy and physical properties in the SAFOD Pilot Hole in Parkfield, CA”, Geophysical Research Letters, Vol 31, doi: 10.1029/2003GL019020, 2004.
[2] Mueller, M. C., “Prediction of lateral variability in fracture intensity using multicomponent shear-wave seismic as a precursor to horizontal drilling”, Geophysical Journal International, Vol 107, pp. 409–415, 1991.
[3] Alford, R. M., “Shear data in the presence of azimuthal anisotropy,” Annual International Meeting of the Society of Exploration Geophysicists Expanded Abstracts, Vol 56, pp.476–479, 1986.
[4] Sayers, C. M., “The elastic anisotropy of shales”, Journal of Geophysical Research, Vol 99, pp. 767–774, 1994.
[5] Boness, N. L., and Zoback, M. D., “Mapping stress and structurally controlled crustal shear velocity anisotropy in California”, Geological Society of America, Vol 34(10), pp. 825-828, 2006a.
[6] Boness, N. L., and Zoback, M. D., “A multiscale study of the mechanisms controlling shear velocity anisotropy in the San Andreas Fault Observatory at Depth”, Geophysics, Vol 71(5), doi:10.1190/1.2231107, 2006b.
[7] 吳泓昱,「車籠埔斷層於台灣大坑井區域之物理參數特性及應力場異質性之模擬」,國立中央大學,博士論文,民國99年。
[8] Hung, J. H., Ma, K. F., Wang, C. Y., Ito, H., Lin, W. and Yeh, E. C., “Subsurface structure, physical properties, fault-zone characteristics and stress state in scientific drill holes of Taiwan Chelungpu Fault Drilling Project”, Tectonophysics, Vol 466, pp. 307–32, 2009.
[9] Louis, L., Chen, N. T. M., David, C., Robion, P., Wong, T. F. and Song, S. R., “Anisotropy of magnetic susceptibility and P-wave velocity in core samples from the Taiwan Chelungpu-Fault Drilling Project (TCDP)”, Journal of Structural Geology, Vol 30, pp. 948–962, 2008.
[10] Louis, L., David, C., Špaček, P., Wong, T. F. Fortin, J. and Song, S. R., “Elastic anisotropy of core samples from the Taiwan Chelungpu Fault Drilling Project (TCDP): direct 3-D measurements and weak anisotropy approximations”, Geophysical Journal International, Vol 188, pp. 239-252, 2012.
[11] Musgrave, M. J. P., Crystal acoustics, Holden-Day, San Francisco, 1971.
[12] Oda, M. “An Experimental Study of the Elasticity of Mylonite Rock with Random Cracks”, International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, Vol 25(2), pp. 59-69, 1988.
[13] Kanatani, K., “Distribution of directional data and fabric tensors”, International Journal of Engineering Science, Vol 22(2), pp. 149-164, 1984.
[14] Oda, M., Modern developments in rock structure characterization, in Compressive Rock Engineering.Vol.1.edited by J. A. Hudson., Elsevier, New York., 1993.
[15] Wu, Y. H., Yeh, E. C., Dong, J. J., Kuo, L. W., Hsu, J. Y. and Hung, J. H., “Core-log integration studies in hole-A of Taiwan Chelungpu-fault Drilling Project”, Geophysical Journal International, Vol 174, pp.949-965, 2008
[16] Asquith, G. and Krygowski, D., Basic well log analysis, second edition, The American Association of Petroleum Geologists, 2004.
[17] Lin, W., Yeh, E. C., Ito, H., Hung, J. H., Hirono, T., Soh, W., Ma, K. F., Kinoshita, M., Wang, C. Y., and Song, S.-R., “Current stress state and principal stress rotations in the vicinity of the Chelungpu fault induced by the 1999 Chi-Chi, Taiwan, earthquake”, Geophysical Research Letters, Vol 34, doi:10.1029/2007GL030515, 2007.
[18] Yeh, E. C., Sone, H., Nakaya, T., Ian, K. H., Song, S. R., Hung, J. H., Lin, W., Hirono, T., Wang, C. Y., Ma, K. F., Soh, W. and Kinoshita, M., “Core description and characteristics of fault zones from Hole-A of the Taiwan Chelungpu-Fault drilling project”, Terrestrial, Atmospheric and Oceanic Sciences, Vol 18(2), pp. 327–357, 2007.
[19] 嚴珮綺,「利用鑽井資料推估台灣新竹至台中地區的地下現地應力狀態」,國立中央大學,碩士論文,民國101年。
[20] Johnston, J. E. and Christensen N. I., “Seismic anisotropy of shales”, Journal of Geophysical Research, Vol 100(4), pp.5991-6003, 1995.
[21] Lin, W., Yeh, E. C., Ito, H., Hirono, T., Soh, W., Wang, C. Y., Ma, K. F., Hung, J. H., and Song, S.-R., “Preliminary results of stress measurement using drill cores of TCDP Hole-A: an application of anelastic strain recovery method to three dimensional in-situ stress determination”, Terrestrial, Atmospheric and Oceanic Sciences, Vol 18(2), pp. 379–393, 2007b.
[22] Yabe, Y., Song, S. R. and Wang, C. Y., ”In-situ stress at the northern portion of the Chelungpu fault, Taiwan, estimated on boring cores recovered from a 2-km-deep hole of TCDP”, Earth Planets Space, Vol 60, pp.809–819., 2008.
[23] Castagna, P., Batzle, M. L., and Eastwood, R. L., “Relationships between compressional-wave and shear-wave velocities in elastic silicate rocks”, Geophysics, Vol 50(4), pp. 571-581, 1985.
[24] 鄭允嘉,「節理岩體滲透係數之先天異向性與應力引致異向性」,國立中央大學,碩士論文,民國95年。
[25] Oda, M., ” An Equivalent Continuum Model for Coupled Stress and Fluid Flow Analysis in Jointed Rock Masses”, Water Resources Research, Vol 22(13), pp. 1845-1856, 1986.
[26] Lee, C. H. and Farmer, I. W., Fluid Flow in Discontinuous Rocks, First Edition. Chapman and Hall, 1993.
[27] International Society For Rock Mechanics, “International society for rock mechanics commission on standardization of laboratory and field test: suggested methods for the quantitative description of discontinuities in rock mass,” International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, Vol 15, pp. 319-368, 1977.
[28] Schlumberger, DSI Dipole Shear Sonic Imager, Schlumberger Marketing Communications, Houston., 2004
[29] 陳正旺,「車籠埔斷層周圍岩石力學特性之初探」,國立台灣大學土木工程學研究所,碩士論文,民國94年。
[30] Cheng, H.C, and Toksoz, M.N., “A three-dimensional model to simulate joint networks in layered rocks,” Canadian Journal of Earth Sciences, Vol 39, pp.1443-1455, 1979.
[31] Zou, Y., Taylor, W. E. G., and Heath, D. J., “A numerical model for borehole breakouts,” International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, Vol 33, pp. 103-109, 1996.
|