Mechanisms of shear localization in the continental lithosphere: inference from the deformation microstructures of peridotites from the Ivrea zone, northwestern Italy
- 31 March 1998
- journal article
- Published by Elsevier BV in Journal of Structural Geology
- Vol. 20 (2-3), 195-209
- https://doi.org/10.1016/s0191-8141(97)00059-x
Abstract
No abstract availableKeywords
Funding Information
- National Science Foundation (EAR-92201 72)
This publication has 47 references indexed in Scilit:
- Flow laws for rocks containing two non-linear viscous phases: A phenomenological approachJournal of Structural Geology, 1994
- Shear localisation in upper mantle peridotitesPure and Applied Geophysics, 1991
- Deformation regimes and the rheological evolution of fault zones in the lithosphere: the effects of pressure, temperature, grainsize and timeTectonophysics, 1989
- Shear band formation in plane strain compressionActa Metallurgica, 1988
- Deep crustal extensional faulting in the Ivrea Zone of Northern ItalyTectonophysics, 1987
- Deformation mechanisms in a high-temperature quartz-feldspar mylonite: evidence for superplastic flow in the lower continental crustTectonophysics, 1987
- On dynamic recrystallisationScripta Metallurgica, 1987
- Stress and temperature in the bending lithosphere as constrained by experimental rock mechanicsGeophysical Journal International, 1979
- The temperature variation of hardness of olivine and its implication for polycrystalline yield stressJournal of Geophysical Research, 1979
- The orthoenstatite to clinoenstatite transformation by shearing and reversion by annealing: Mechanism and potential applicationsBeiträge zur Mineralogie und Petrographie, 1975