Strain and strain rate in a synkinematic trondhjemitic dike: evidence for melt-induced strain softening during shearing (Bohemian Massif, Czech Republic)
- 1 May 1997
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 19 (5) , 639-652
- https://doi.org/10.1016/s0191-8141(96)00100-9
Abstract
No abstract availableKeywords
This publication has 52 references indexed in Scilit:
- Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear ZonePublished by Elsevier ,2003
- Fabric development in shear zones: theoretical controls and observed phenomenaPublished by Elsevier ,2003
- Rates of processes in magmatic arcs: implications for the timing and nature of pluton emplacement and wall rock deformationPublished by Elsevier ,2003
- Structural evidence for the relationship between thrusts, extensional faults and granite intrusions in the Variscan belt of Galicia (Spain)Published by Elsevier ,2003
- Microstructures in feldspars from a major crustal thrust zone: The Grenville Front, Ontario, CanadaPublished by Elsevier ,2003
- The case for simultaneous deformation, metamorphism and plutonism: an example from Proterozoic rocks in central ArizonaJournal of Structural Geology, 1995
- Re-examining pluton emplacement processesJournal of Structural Geology, 1993
- Diffusion creep in feldspar aggregates: experimental evidenceJournal of Structural Geology, 1991
- Local variations in quartz [c]-axis orientations in non-coaxial regimes and their significance for the mechanics of S-C fabricsJournal of Structural Geology, 1990
- Two-dimensional strain from the orientation of lines in a planeJournal of Structural Geology, 1984