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Bulletin of the Seismological Society of America; August 1985; v. 75; no. 4; p. 1135-1154
© 1985 Seismological Society of America
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Surface deformation due to shear and tensile faults in a half-space

YOSHIMITSU OKADA*

LAMONT-DOHERTY GEOLOGICAL OBSERVATORY OF COLUMBIA UNIVERSITY, PALISADES, NEW YORK 10964

Abstract

A complete suite of closed analytical expressions is presented for the surface displacements, strains, and tilts due to inclined shear and tensile faults in a half-space for both point and finite rectangular sources. These expressions are particularly compact and free from field singular points which are inherent in the previously stated expressions of certain cases. The expressions derived here represent powerful tools not only for the analysis of static field changes associated with earthquake occurrence but also for the modeling of deformation fields arising from fluid-driven crack sources.

Footnotes

* Present address: National Research Center for Disaster Prevention, Science and Technology Agency, Sakura-mura, Ibaraki, 305 Japan.




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Rapid Deformation of the South Flank of Kilauea Volcano, Hawaii
Science, March 3, 1995; 267(5202): 1328 - 1332.
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K. W. Hudnut, Y. Bock, M. Cline, P. Fang, Y. Feng, J. Freymueller, X. Ge, W. K. Gross, D. Jackson, M. Kim, et al.
Co-seismic displacements of the 1992 landers earthquake sequence
Bulletin of the Seismological Society of America, June 1, 1994; 84(3): 625 - 645.
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H. O. Johnson, D. C. Agnew, and K. Hudnut
Extremal bounds on earthquake movement from geodetic data: Application to the Landers earthquake
Bulletin of the Seismological Society of America, June 1, 1994; 84(3): 660 - 667.
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M. J. S. Johnston, A. T. Linde, and D. C. Agnew
Continuous borehole strain in the San Andreas fault zone before, during, and after the 28 June 1992, MW 7.3 Landers, California, earthquake
Bulletin of the Seismological Society of America, June 1, 1994; 84(3): 799 - 805.
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L. B. Grant and A. Donnellan
1855 and 1991 surveys of the San Andreas fault: Implications for fault mechanics
Bulletin of the Seismological Society of America, April 1, 1994; 84(2): 241 - 246.
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T. ARNDOTTIR, P. SEGALL, and M. MATTHEWS
Resolving the discrepancy between geodetic and seismic fault models for the 1989 Loma Prieta, California, earthquake
Bulletin of the Seismological Society of America, October 1, 1992; 82(5): 2248 - 2255.
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K. SATAKE and P. G. SOMERVILLE
Location and size of the 1927 Lompoc, California, earthquake from tsunami data
Bulletin of the Seismological Society of America, August 1, 1992; 82(4): 1710 - 1725.
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Y. DU, A. AYDIN, and P. SEGALL
Comparison of various inversion techniques as applied to the determination of a geophysical deformation model for the 1983 Borah Peak earthquake
Bulletin of the Seismological Society of America, August 1, 1992; 82(4): 1840 - 1866.
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Y. OKADA
Internal deformation due to shear and tensile faults in a half-space
Bulletin of the Seismological Society of America, April 1, 1992; 82(2): 1018 - 1040.
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R. A. SNAY, H. C. NEUGEBAUER, and W. H. PRESCOTT
Horizontal deformation associated with the Loma Prieta earthquake
Bulletin of the Seismological Society of America, October 1, 1991; 81(5): 1647 - 1659.
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P. T. Delaney, P. T. Delaney, R. S. Fiske, A. Miklius, A. T. Okamura, and M. K. Sako
Deep Magma Body Beneath the Summit and Rift Zones of Kilauea Volcano, Hawaii
Science, March 16, 1990; 247(4948): 1311 - 1316.
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N. E. KING, D. C. AGNEW, and F. WYATT
Comparing strain events: A case study for the Homestead Valley earthquakes
Bulletin of the Seismological Society of America, October 1, 1988; 78(5): 1693 - 1706.
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S. E. BARRIENTOS, R. S. STEIN, and S. N. WARD
Comparison of the 1959 Hebgen Lake, Montana and the 1983 Borah Peak, Idaho, earthquakes from geodetic observations
Bulletin of the Seismological Society of America, June 1, 1987; 77(3): 784 - 808.
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null Yang Xue-Min, X.-M. YANG, and P. M. DAVIS
Deformation due to a rectangular tension crack in an elastic half-space
Bulletin of the Seismological Society of America, June 1, 1986; 76(3): 865 - 881.
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H. Dragert, K. Wang, and T. S. James
A Silent Slip Event on the Deeper Cascadia Subduction Interface
Science, May 25, 2001; 292(5521): 1525 - 1528.
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