Flow strengths of quartz aggregates: Grain size and pressure effects due to hydrolytic weakening
- 10 June 1984
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 89 (B6), 4281-4297
- https://doi.org/10.1029/jb089ib06p04281
Abstract
No abstract availableKeywords
This publication has 37 references indexed in Scilit:
- Grain Growth Kinetics of Quartz and Calcite AggregatesThe Journal of Geology, 1982
- A deformed polymictic conglomerate—the influence of grain size and composition on the mechanism and rate of deformationTectonophysics, 1981
- The influence of metamorphic environment upon the deformation of mineralsTectonophysics, 1981
- Distribution of impurities in deformed quartz and its implications for deformation studiesTectonophysics, 1980
- Grain-size sensitive deformation of a stretched conglomerate from Plymouth, VermontJournal of Structural Geology, 1980
- Superplastic flow in finegrained limestoneTectonophysics, 1977
- Finite-element folds of similar geometryTectonophysics, 1976
- Rheological evidence for changes in the deformation mechanism of Solenhofen limestone towards low stressesTectonophysics, 1976
- Microstructure of mylonites and their descriptive terminologyLithos, 1973
- Experimentally induced 'natural' intragranular flow in quartz and quartziteAmerican Journal of Science, 1968