| Citation: |
FENG RUIup, T. V. MCEVILLYup2com s. 1984: INTERPRETATION OF SEISMIC REFLECTION PROFILING DATA FOR THE STRUCTURE OF THE SAN ANDREAS FAULT ZONE. Acta Seismologica Sinica, 6(3): 249-263.
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[1] Aki, K. and Lee, W. H. K., Determination of three——dimensional velocity anomalies under a seismic array using P——arrival times from local earthquakes: 1. A homogeneous initial model, J. Geophys.Res., 23, 4381——4399, 1976.
[2] Aric,K., Gutdeutsch, R,and Sailer, A., Computation of travel times and rays in a medium of two——dimensional velocity distribution, Pageoph, 118, 796——806, 1980. [3] Boore, D. M. and Hill,D. P., Wave propagation characteristics in the vicinity of the San Andreas Fault, Proceedings of the Conference on Tectonic Problems of the San Andreas Fault System, Stan——ford Univ. Publ., 13, 215——224, 1973. [4] Chauqui, L. and McEvilly, T. V., Detailed crustal structure within the central California large——scale.seismic array, in Annual Report, Seismographic Station, University of California, Berkeley, 1968. [5] Clymer, R. W. and McEvilly. T. V., Travel——time monitoring with VIBROSEIS, Bul乙Seism. Soc. Am.71, 1902——1927, 1981. [6] Eaton, J. P., Lee, W. H. K. and Pakiser, L. C., Use of microearthquakes in the study of the me——chanics of earthquake generation along the San Andreas fault in central California, Tectonophysics, 9,259——282, 1970. [7] Engdahl, E. R. and Lee, W. H. K., Relocation of local earthquakes by seismic ray tracing,J. Geophys.Res, 81, 4400——4406, 1976. [8] Ellsworth, W. L., Bear Valley, California, earthquake sequence of February——March 1972, Bull. Seism Soc. Am, 65 483——506, 1975. [9] Healy, J. and Peake, L., Seismic veloeity structure along a section of the Andreas fault near Bear Valley, California, Bull. Seism. Soc. Am, 65, 1177——1197, 1975, [10] Lin, W. and Wang, C. Y., P——wave velocities in rocks at high pressure and temperature and the constitution of the central California crust, Geophy. J. R. Astr. Soc, 61, 379——400, 1980. [11] May, B. T. and Covey, J. D., An inverse ray method for computing geologic structures from seismic reflections——Zero——offset case, Geophysics, 46, 268——2$7, 1981. [12] McEvilly,T. V,Crustal structure estimation within a large scale array, Geophys.].R. Astr. Soc, 11,13——17, 1966. [13] McEvilly, T. V., Extended reflection survey of the San Andreas fault zone, U. S. Geol. Sutv. Open——File Report No. 81——388, 1981. [14] McEvilly, T. V. and Clymer, R. W., A deep crustal reflection survey on the San Andreas fault, EOS Trans. Am. Geophys. Union 56, 1021, 1975. [15] McLaughlin, K. L., Spatial coherency of seismic waveforms, Ph, D. Thesis, Univ. of California, Ber.keley, 1982. [16] McNally, K. C. and McEvilly, T. V., Velocity contrast across the San Andreas fault in central Cali——forma: small——scale variation from P——wave nodal plane distortion, Bull. Seism. Soc. Am, 67, 1565——1576, 1977. [17] Mooney, W. D. and Luetgert, J. H., A seismic refraction study of the Santa Clara Valley and Southern Santa Cruz mountains, West——central California, Bxa1l. Seism. Soc. Am. 72, 901——909, 1982. [18] Walter, A. W. and Mooney, W. D., Crustal structure of the Diablo and Gabilan ranges, central Cali——fotnia:. a reinterpretation of existing data, Bull. Seism. Soc. Am, 72, 1567——1590. 1982. [19] Stierman, D. J. and Zappe, S. D., Lateral P——velocity gradients near major strike——slip faults in Cali——forma, Science, 213, 207——209, 1981. [20] Wang, C. Y:, Lin, W. and Wu, F. T., Constitution of the San Andreas fault zone at depth, Geophys.Res. Lett, 5, 741, 1978. [21] Wesson, R. L., Travel——time inversion for laterally inhomogeneous crustal velocity models, Bull. Seism.Soc. Am., 61, 729——746, 1971.
[1] Aki, K. and Lee, W. H. K., Determination of three——dimensional velocity anomalies under a seismic array using P——arrival times from local earthquakes: 1. A homogeneous initial model, J. Geophys.Res., 23, 4381——4399, 1976.
[2] Aric,K., Gutdeutsch, R,and Sailer, A., Computation of travel times and rays in a medium of two——dimensional velocity distribution, Pageoph, 118, 796——806, 1980. [3] Boore, D. M. and Hill,D. P., Wave propagation characteristics in the vicinity of the San Andreas Fault, Proceedings of the Conference on Tectonic Problems of the San Andreas Fault System, Stan——ford Univ. Publ., 13, 215——224, 1973. [4] Chauqui, L. and McEvilly, T. V., Detailed crustal structure within the central California large——scale.seismic array, in Annual Report, Seismographic Station, University of California, Berkeley, 1968. [5] Clymer, R. W. and McEvilly. T. V., Travel——time monitoring with VIBROSEIS, Bul乙Seism. Soc. Am.71, 1902——1927, 1981. [6] Eaton, J. P., Lee, W. H. K. and Pakiser, L. C., Use of microearthquakes in the study of the me——chanics of earthquake generation along the San Andreas fault in central California, Tectonophysics, 9,259——282, 1970. [7] Engdahl, E. R. and Lee, W. H. K., Relocation of local earthquakes by seismic ray tracing,J. Geophys.Res, 81, 4400——4406, 1976. [8] Ellsworth, W. L., Bear Valley, California, earthquake sequence of February——March 1972, Bull. Seism Soc. Am, 65 483——506, 1975. [9] Healy, J. and Peake, L., Seismic veloeity structure along a section of the Andreas fault near Bear Valley, California, Bull. Seism. Soc. Am, 65, 1177——1197, 1975, [10] Lin, W. and Wang, C. Y., P——wave velocities in rocks at high pressure and temperature and the constitution of the central California crust, Geophy. J. R. Astr. Soc, 61, 379——400, 1980. [11] May, B. T. and Covey, J. D., An inverse ray method for computing geologic structures from seismic reflections——Zero——offset case, Geophysics, 46, 268——2$7, 1981. [12] McEvilly,T. V,Crustal structure estimation within a large scale array, Geophys.].R. Astr. Soc, 11,13——17, 1966. [13] McEvilly, T. V., Extended reflection survey of the San Andreas fault zone, U. S. Geol. Sutv. Open——File Report No. 81——388, 1981. [14] McEvilly, T. V. and Clymer, R. W., A deep crustal reflection survey on the San Andreas fault, EOS Trans. Am. Geophys. Union 56, 1021, 1975. [15] McLaughlin, K. L., Spatial coherency of seismic waveforms, Ph, D. Thesis, Univ. of California, Ber.keley, 1982. [16] McNally, K. C. and McEvilly, T. V., Velocity contrast across the San Andreas fault in central Cali——forma: small——scale variation from P——wave nodal plane distortion, Bull. Seism. Soc. Am, 67, 1565——1576, 1977. [17] Mooney, W. D. and Luetgert, J. H., A seismic refraction study of the Santa Clara Valley and Southern Santa Cruz mountains, West——central California, Bxa1l. Seism. Soc. Am. 72, 901——909, 1982. [18] Walter, A. W. and Mooney, W. D., Crustal structure of the Diablo and Gabilan ranges, central Cali——fotnia:. a reinterpretation of existing data, Bull. Seism. Soc. Am, 72, 1567——1590. 1982. [19] Stierman, D. J. and Zappe, S. D., Lateral P——velocity gradients near major strike——slip faults in Cali——forma, Science, 213, 207——209, 1981. [20] Wang, C. Y:, Lin, W. and Wu, F. T., Constitution of the San Andreas fault zone at depth, Geophys.Res. Lett, 5, 741, 1978. [21] Wesson, R. L., Travel——time inversion for laterally inhomogeneous crustal velocity models, Bull. Seism.Soc. Am., 61, 729——746, 1971. |
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