Crustal deformation is the study of active geophysical processes that occur within he earth’s lithosphere. Geodesy provides facilities to investigate the earth’s crust ovements and shares these data with the other disciplines. The various sources ...

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 ...

A two-layer (crust and upper mantle), finite difference steady-state thermomechanical model of a long-lived (several million years) lithospheric strike-slip fault is presented, and its predictions compared with field observations from various major fault zones ...