variations and fluid circulation in a deep shear zone: The case of the Alpine ultramylonites from the Aar massif (Central Alps, Switzerland)
- 5 October 1989
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 77 (2) , 119-131
- https://doi.org/10.1016/0009-2541(89)90137-x
Abstract
No abstract availableKeywords
This publication has 35 references indexed in Scilit:
- Strain pattern in the Aar Granite (Central Alps): Orthogneiss developed by bulk inhomogeneous flatteningPublished by Elsevier ,2003
- Bulk kinematics from shear zone patterns: some field examplesJournal of Structural Geology, 1987
- Thermal and fluid regimes in the Bitterroot lobe–Sapphire block detachment zone, Montana: Evidence from 18O/16O and geologic relationsGSA Bulletin, 1986
- The Lepontine Alps as an evolving metamorphic core complex during a‐type subduction: Evidence from heat flow, mineral cooling ages, and tectonic modelingTectonics, 1985
- Reaction softening in mylonites from the Arnaboll thrust, SutherlandScottish Journal of Geology, 1983
- Reaction and Geometrical Softening in Granitoid MylonitesTexture, Stress, and Microstructure, 1982
- A Discussion on natural strain and geological structure - Pressure-solution and crystallization deformationPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1976
- A Discussion on global tectonics in Proterozoic times - The interrelations of fluid transport, deformation, geochemistry and heat flow in early Proterozoic shear zones in the Lewisian complexPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1976
- Oxygen isotope partitioning among the minerals in igneous and metamorphic rocksReviews of Geophysics, 1975
- Chemical changes during retrogressive metamorphism of Lewisian granulite facies rocks from Coll and TireeScottish Journal of Geology, 1974