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Surface deformation due to shear and tensile faults in a half-space
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.
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Cited by
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The 2010 M w 8.8 Maule Megathrust Earthquake of Central Chile, Monitored by GPS
Vigny, C., Socquet, A., Peyrat, S., Ruegg, J.-C., Métois, M., Madariaga, R., Morvan, S., Lancieri, M., Lacassin, R., Campos, J., et al. (2011) · Science · doi:10.1126/science.1204132 · Cited by 414
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Larson, K. M., Bürgmann, R., Bilham, R., & Freymueller, J. T. (1999) · Journal of Geophysical Research: Solid Earth · doi:10.1029/1998jb900043 · Cited by 381
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The volcano–seismic crisis in Afar, Ethiopia, starting September 2005
Ayele, A., Jacques, E., Kassim, M., Kidane, T., Omar, A., Tait, S., Nercessian, A., de Chabalier, J.-B., & King, G. (2007) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2006.12.014 · Cited by 133
Metadata
- Authors
- Okada, Y.
- Venue
- Bulletin of the Seismological Society of America
- Published
- 1985-08-01
- Volume
- 75
- Issue
- 4
- Pages
- 1135-1154
- ISSN
- 0037-1106 (ISSN-L)
- 1943-3573
- OpenAlex
- W2124799255
- Cited by
- 5,169
- References
- 0
- FWCI
- 4.67
- Type
- journal article
- Language
- en
- Open access
- closed
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- Okada, Y. (1985). Surface deformation due to shear and tensile faults in a half-space. Bulletin of the Seismological Society of America. https://doi.org/10.1785/bssa0750041135
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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