The brittle‐plastic transition in experimentally deformed quartz aggregates
- 10 June 1994
- journal article
- research article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Solid Earth
- Vol. 99 (B6), 11731-11747
- https://doi.org/10.1029/93jb02873
Abstract
No abstract availableKeywords
This publication has 62 references indexed in Scilit:
- The role of dynamic recrystallization in the development of lattice preferred orientations in experimentally deformed quartz aggregatesJournal of Structural Geology, 1993
- Lithosphere strength inferred from fracture strength of rocks at high confining pressures and temperaturesTectonophysics, 1993
- Deformation mechanisms accommodating faulting of quartzite under upper crustal conditionsJournal of Structural Geology, 1992
- Dislocation creep regimes in quartz aggregatesJournal of Structural Geology, 1992
- Fourier transform infrared spectroscopy determinations of intragranular water content in quartz-bearing rocks: implications for hydrolytic weakening in the laboratory and within the earthTectonophysics, 1990
- Stress estimates and fault history from quartz microstructuresJournal of Structural Geology, 1988
- Deformation mechanisms in granitic rocks at shallow crustal levelsJournal of Structural Geology, 1988
- Microcracks in rocks: A reviewTectonophysics, 1983
- Friction in faulted rock at high temperature and pressureTectonophysics, 1974
- Experimentally induced 'natural' intragranular flow in quartz and quartziteAmerican Journal of Science, 1968