Dependence on the elastic constants of surface deformation due to faulting

Author:

Converse Glenn1,Comninou Maria2

Affiliation:

1. U.S. Geological Survey Menlo Park, California

2. Department of Applied Mechanics and Engineering Science University of Michigan Ann Arbor, Michigan

Abstract

Abstract In general, the explicit expressions for surface displacements calculated from dislocation models of faulting in a half-space are restricted to the case λ = μ, where λ and μ are the Lamé elastic constants (e.g., Maruyama, 1964; Press, 1965; Mansinha and Smylie, 1971). It is obviously of some interest to know how the surface fields might be modified by other choices of the elastic constants. In this paper it is shown that the surface displacements depend upon the elastic constants only as linear functions of the Poisson ratio v. The intercepts and slopes of the linear functions, of course, vary with position on the free surface. The surface tilts and strains are also simple functions of the Poisson ratio.

Publisher

Seismological Society of America (SSA)

Subject

Geochemistry and Petrology,Geophysics

Cited by 3 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. Recent Geodynamics of Induced Faults;Izvestiya, Atmospheric and Oceanic Physics;2023-12

2. Recent Volumetric Deformations of Fault Zones;Izvestiya, Physics of the Solid Earth;2022-08

3. Deformation Consequences of the Development оf Oil and Gas Field;Izvestiya, Atmospheric and Oceanic Physics;2021-12

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