Constraining the P–T path of (U)HP rocks with reaction overstepping during subduction; example from the Western Gneiss Region (Norway)
Author:
Affiliation:
1. Faculty of Science, Institute of Petrology and Structural Geology Charles University Prague 2 Czech Republic
2. Faculty of Science, Institute of Applied Mathematics and Information Technology Charles University Prague Czech Republic
Funder
Grantová Agentura České Republiky
FP7 Cooperation
Univerzita Karlova v Praze
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12680
Reference97 articles.
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3. Processing of crust in the root of the Caledonian continental collision zone: the role of eclogitization
4. A ternary feldspar-mixing model based on calorimetric data: development and application
5. A four‐phase model for the Sveconorwegian orogeny, SW Scandinavia;Bingen B.;Norsk Geologisk Tidsskrift,2008
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