The relationship between slickenside surfaces in fine-grained quartz and the seismic cycle
- 1 January 1989
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 11 (7) , 879-893
- https://doi.org/10.1016/0191-8141(89)90105-3
Abstract
No abstract availableKeywords
This publication has 52 references indexed in Scilit:
- Crack-seal fibre growth mechanisms and their significance in the development of oriented layer silicate microstructuresPublished by Elsevier ,2003
- Determination of the mean principal directions of stresses for a given fault populationPublished by Elsevier ,2003
- Crystal growth in cataclasites: Diagnostic microstructures and implicationsPublished by Elsevier ,2003
- Criteria for the sense of movement on fault surfaces in brittle rocksPublished by Elsevier ,2003
- Kinematic indicators on active normal faults in Western TurkeyPublished by Elsevier ,2003
- Experimentally produced slickenside lineations in pyrophyllitic clayJournal of Structural Geology, 1989
- A newly recognized type of slickenside striationJournal of Structural Geology, 1987
- Deformation within foreland thrust sheets by populations of minor faultsJournal of Structural Geology, 1986
- Deformation of granitic rocks across the brittle-ductile transitionJournal of Structural Geology, 1985
- The simulation of fabric development in plastic deformation and its application to quartzite: The modelTectonophysics, 1978