Partially open grain and phase boundaries as fluid pathways in metamorphic and magmatic rocks-Reference-Cited by-同舟云学术

Partially open grain and phase boundaries as fluid pathways in metamorphic and magmatic rocks

Published:2021-07-28 Issue:1 Volume:40 Page:67-85
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:Journal Metamorphic Geology

Author:

Wirth Richard¹,Kruhl Jörn H.²³^ORCID,Morales Luiz F. G.⁴,Schreiber Anja¹

Affiliation:

1. Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences Potsdam Germany

2. Department of Earth and Environmental Sciences Ludwig‐Maximilians‐Universität München Munich Germany

3. Faculty of Civil, Geo and Environmental Engineering Technische Universität München Munich Germany

4. Scientific Center for Optical and Electron Microscopy (ScopeM) Zürich Switzerland

Funder

Deutsche Forschungsgemeinschaft

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12610

Reference72 articles.

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3. Instantaneous rock transformations in the deep crust driven by reactive fluid flow

4. Grain boundary dissolution porosity in quartzofeldspathic ultramylonites: Implications for permeability enhancement and weakening of mid-crustal shear zones

5. Precise determinations of the equilibria kyanite ‐ sillimanite and kyanite ‐ andalusite and a revised triple point for Al2SiO5 polymorphs;Bohlen S. R.;American Mineralogist,1991

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