Quartz dislocation microstructure between 7000 m and 9100 m depth from the Continental Deep Drilling Program KTB
- 10 August 1997
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Solid Earth
- Vol. 102 (B8), 18443-18452
- https://doi.org/10.1029/96jb03394
Abstract
No abstract availableKeywords
This publication has 44 references indexed in Scilit:
- Post‐Variscan thermal and tectonic evolution of the KTB site and its surroundingsJournal of Geophysical Research, 1997
- Estimation of the complete stress tensor to 8 km depth in the KTB scientific drill holes: Implications for crustal strengthJournal of Geophysical Research, 1997
- A flow law for dislocation creep of quartz aggregates determined with the molten salt cellTectonophysics, 1995
- Dislocation creep regimes in quartz aggregatesJournal of Structural Geology, 1992
- Flow properties of continental lithosphereTectonophysics, 1987
- Problems in the extrapolation of laboratory rheological dataTectonophysics, 1987
- Rheological stratification of the lithosphereTectonophysics, 1987
- Deformation of granitic rocks across the brittle-ductile transitionJournal of Structural Geology, 1985
- Hydrolytic weakening of experimentally deformed Westerly granite and Hale albite rockJournal of Structural Geology, 1980
- Estimates of differential stress recorded in the dislocation structure of Lochseiten Limestone (Switzerland)Tectonophysics, 1978