Evolution of synmetamorphic veins and their wallrocks through a Western Alps transect: no evidence for large-scale fluid flow. Stable isotope, major- and trace-element systematics
- 1 January 1996
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 127 (1-3) , 81-109
- https://doi.org/10.1016/0009-2541(95)00106-9
Abstract
No abstract availableKeywords
This publication has 72 references indexed in Scilit:
- The spots and stains of plate tectonicsPublished by Elsevier ,2003
- Metasomatism during subduction: products and possible paths in the Catalina Schist, CaliforniaPublished 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
- Silica mobility and fluid movement during metamorphism of the Connemara schists, IrelandJournal of Metamorphic Geology, 1992
- The origin of the Kupferschiefer-type mineralization in the Richelsdorf Hills, Germany, as deduced from stable isotope and organic geochemical studiesChemical Geology, 1991
- Fluid transport in lineamentsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1986
- 1984 Compilation of Working Values and Sample Description for 170 International Reference Samples Of Mainly Silicate Rocks and MineralsGeostandards Newsletter, 1984
- Quartz veins and devolatilization during metamorphismJournal of the Geological Society, 1983
- Oxygen-isotope equilibration and permeability enhancement during regional metamorphismJournal of the Geological Society, 1983
- The crystal structure of ferrocarpholiteActa Crystallographica, 1956