Textures of sheared halite and their implications for the seismogenic slip of deep faults
- 15 December 1987
- journal article
- research article
- Published by Elsevier in Tectonophysics
- Vol. 144 (1-3) , 69-86
- https://doi.org/10.1016/0040-1951(87)90009-6
Abstract
No abstract availableThis publication has 18 references indexed in Scilit:
- Experimental folding and faulting of rocks under confining pressure Part IX. Wrench faults in limestone layersPublished by Elsevier ,2003
- Transition Between Frictional Slip and Ductile Flow for Halite Shear Zones at Room TemperatureScience, 1986
- The origin of large or great thrust-type earthquakes along subducting plate boundariesTectonophysics, 1985
- Laboratory friction experiments and natural earthquakes: An argument for long-term testsTectonophysics, 1984
- Why large earthquakes do not nucleate at shallow depthsNature, 1983
- Continental fault structure and the shallow earthquake sourceJournal of the Geological Society, 1983
- Limits of stresses in continental crusts and their relation to the depth‐frequency distribution of shallow earthquakesTectonics, 1982
- Specimen-apparatus interaction during stick-slip in a tri axial compression machine: A decoupled two-degree-of-freedom modelTectonophysics, 1980
- Structures developed in fault gouge during stable sliding and stick-slipTectonophysics, 1978
- Fault rocks and fault mechanismsJournal of the Geological Society, 1977