Strain accommodation about strike-slip fault discontinuities in granitic rock under brittle-to-ductile conditions
- 31 March 2003
- journal article
- research article
- Published by Elsevier
- Vol. 16 (12) , 1655-1674
- https://doi.org/10.1016/0191-8141(94)90133-3
Abstract
No abstract availableThis publication has 66 references indexed in Scilit:
- Fault geometries in basement-induced wrench faulting under different initial stress statesPublished by Elsevier ,2003
- Strike-slip duplexesPublished by Elsevier ,2003
- Hydrolytic weakening of experimentally deformed Westerly granite and Hale albite rockPublished by Elsevier ,2003
- Pseudotachylyte-bearing strike-slip duplex structures in the Fort Foster Brittle Zone, S. MainePublished by Elsevier ,2003
- Duplex structures connecting fault segments in Entrada SandstoneJournal of Structural Geology, 1991
- Nucleation and growth of retrograde shear zones: an example from the Needle Mountains, Colorado, U.S.A.Journal of Structural Geology, 1990
- On the formation and growth of faults: an experimental studyJournal of Structural Geology, 1988
- Bridge structures as sense of displacement criteria in brittle fault zonesJournal of Structural Geology, 1987
- Experimental fracture, strain and subsidence patterns over en échelon strike-slip faults: implications for the structural evolution of pull-apart basinsJournal of Structural Geology, 1986
- Deformation of granitic rocks across the brittle-ductile transitionJournal of Structural Geology, 1985