Granite emplacement during contemporary shortening and normal faulting: structural and magnetic study of the Veiga Massif (NW Spain)
- 27 December 1995
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 17 (12), 1689-1706
- https://doi.org/10.1016/0191-8141(95)00062-i
Abstract
No abstract availableKeywords
This publication has 41 references indexed in Scilit:
- The maladeta granite polydiapir, Spanish Pyrenees: A detailed magnetostructural studyJournal of Structural Geology, 1994
- Structural evidence for the relationship between thrusts, extensional faults and granite intrusions in the Variscan belt of Galicia (Spain)Journal of Structural Geology, 1992
- Magnetic susceptibility of the rock matrix related to magnetic fabric studiesJournal of Structural Geology, 1987
- Structural pattern and ascent model in the Central Extremadura batholith, Hercynian belt, SpainJournal of Structural Geology, 1986
- Structural, metamorphic and magmatic history of the Mondon̄edo nappe (Hercynian belt, NW Spain)Journal of Structural Geology, 1986
- Deformation of granitic rocks across the brittle-ductile transitionJournal of Structural Geology, 1985
- Strain patterns of pluton emplacement in a crust undergoing non-coaxial deformation, Sierra Morena, Southern SpainJournal of Structural Geology, 1981
- Shear zones in the iberian arcJournal of Structural Geology, 1980
- Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear ZoneJournal of Structural Geology, 1979
- Fabric development in shear zones: theoretical controls and observed phenomenaJournal of Structural Geology, 1979