Earth Structure¶
Marshak, S. (2003). Earth Structure: An Introduction to Structural Geology and Tectonics. Earth Structure: An Introduction to Structural Geology and Tectonics.
Cited by¶
2 citations across 2 artifacts.
Each citation links to the sentence it supports in the citing article.
Domain-specific¶
- Erosion and tectonics
- Orogenic Belt
- The defining process is the progressive transfer of compressional stress into the crust as the plates converge: at the surface and in the cool upper crust, this stress is accommodated by brittle faulting — thrust faults and reverse faults that stack crustal slices in an imbricated geometry, thickening the crust to two or more times its pre-collisional value
This sourceThe structural-geology text's definition of brittle faulting along a single discrete surface, and its note that brittle and ductile deformation can occur together.
Supported in partVerified against the work's full text
“[Brittle] fault A single [surface] on which movement occurs specifically by [brittle] deformation”
- The defining process is the progressive transfer of compressional stress into the crust as the plates converge: at the surface and in the cool upper crust, this stress is accommodated by brittle faulting — thrust faults and reverse faults that stack crustal slices in an imbricated geometry, thickening the crust to two or more times its pre-collisional value
Verification¶
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Registry ID ref:0bd5375ff939 · see in the full table