Applications of geophysical inverse theory to faulting and dike intrusion
Surface deformation in the form of length, angle and elevation changes recorded by geodetic networks are inverted to determine slip and opening at depth using geophysical inverse theory. The forward model is based on three-dimensional elastic dislocation theory in a homogeneous isotropic half space....
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| Language: | English |
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Purdue University
1991
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| Online Access: | https://docs.lib.purdue.edu/dissertations/AAI9201319 |