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CRUSTAL BLOCK ROTATIONS AND PLATE COUPLING (2002)
Partitioning of slip at oblique subduction zones is common and frequently results in lithospheric blocks being detached from the overriding plate. A method is described to solve simultaneously for both block rotations on asphere and locking on block-bounding faults using GPS vectors and other geophysical data.
Reference:
AGU Monograph, Plate Boundary Zones, in press.
AGU Monograph, Plate Boundary Zones, in press.
Organization:
Department of Earth and Environmental Sciences, Rensselaer Polytechnic Institute, Troy NY
Department of Earth and Environmental Sciences, Rensselaer Polytechnic Institute, Troy NY
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