Structural evidence for the relationship between thrusts, extensional faults and granite intrusions in the Variscan belt of Galicia (Spain)
- 7 April 2003
- journal article
- Published by Elsevier
- Vol. 14 (10) , 1229-1237
- https://doi.org/10.1016/0191-8141(92)90072-5
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- Shear criteria in granite and migmatite deformed in the magmatic and solid statesPublished by Elsevier ,2003
- C-slip in quartz from subsolidus deformed granitePublished by Elsevier ,2003
- Deformation of leucogranites of the crystalline Main Central Sheet in southern Tibet (China)Published by Elsevier ,2003
- Prism 〈c〉 slip in the quartzites of the Oakhurst Mylonite Belt, CaliforniaJournal of Structural Geology, 1991
- Crustal-scale extension in a convergent orogen : the Sterzing-Steinach mylomte zone in the Eastern AlpsGeodinamica Acta, 1988
- The influence of crystallographic orientation and grain boundary migration on microstructural and textural evolution in an S-C myloniteTectonophysics, 1987
- Structural, metamorphic and magmatic history of the Mondon̄edo nappe (Hercynian belt, NW Spain)Journal of Structural Geology, 1986
- Strain trajectories above the Main Central Thrust (Himalaya) in southern TibetNature, 1985
- Fabric asymmetry and shear sense in movement zonesInternational Journal of Earth Sciences, 1983
- Tibetan, Variscan, and Precambrian Basement Reactivation: Products of Continental CollisionThe Journal of Geology, 1973