Relative motion across the eastern Tibetan plateau: Contributions from faulting, internal strain and rotation rates
A kinematic model comprising 14 rotating, elastic–plastic blocks is used to represent the modern deformation of eastern Tibet and neighboring regions. Block rotations, fault slip rates and permanent strain rates within the blocks are constrained by inverting GPS velocities, slip vector azimuths deri...
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Veröffentlicht in: | Tectonophysics 2013-01, Vol.584, p.240-256 |
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Format: | Artikel |
Sprache: | eng |
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