Interdependence of deformation, fluid infiltration and reaction progress recorded in eclogitic metagranitoids (Sesia Zone, Western Alps)
- 5 May 1994
- journal article
- Published by Wiley in Journal of Metamorphic Geology
- Vol. 12 (3) , 327-343
- https://doi.org/10.1111/j.1525-1314.1994.tb00026.x
Abstract
No abstract availableKeywords
This publication has 55 references indexed in Scilit:
- Geochemistry, geochronology and petrology of Monte Mucrone: An example of EO-alpine eclogitization of Permian granitoids in the Sesia-Lanzo Zone, Western Alps, ItalyPublished by Elsevier ,2004
- Hydrolytic weakening of experimentally deformed Westerly granite and Hale albite rockPublished by Elsevier ,2003
- Fluid circulation, progressive deformation and mass-transfer processes in the upper crust: the example of basement-cover relationships in the External Crystalline Massifs, SwitzerlandJournal of Structural Geology, 1992
- Deformation and recrystallization mechanisms in naturally deformed omphacites from the Sesia-Lanzo zone; geophysical consequencesTectonophysics, 1991
- Migration of reaction and isotopic fronts in infiltration zones: assessments of fluid flux in metamorphic terrainsEarth and Planetary Science Letters, 1990
- Advective-diffusive transport of isotopic fronts: An example from Naxos, GreeceEarth and Planetary Science Letters, 1990
- Carbon and oxygen isotopes in eclogites, amphibolites, veins and marbles from the Western Gneiss region, NorwayChemical Geology: Isotope Geoscience section, 1985
- A Thermal-Tectonic Model for High-Pressure Metamorphism and Deformation in the Sesia Zone, Western AlpsThe Journal of Geology, 1984
- Reaction-enhanced ductility: The role of solid-solid univariant reactions in deformation of the crust and mantleTectonophysics, 1983
- Grain Growth Kinetics of Quartz and Calcite AggregatesThe Journal of Geology, 1982