A THIN VISCOUS SHEET MODEL FOR CONTINENTAL DEFORMATION
For the purposes of describing its large-scale and long-term deformation, the continental lithosphere is regarded as a continuum, obeying a Newtonian or a power law rheology. The flow of a thin sheet of power law material overlying an inviscid substrate is studied under the assumption that vertical...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
| Published: |
1982
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