Phase equilibria modelling constraints on P–T conditions during fluid catalysed conversion of granulite to eclogite in the Bergen Arcs, Norway-Reference-Cited by-同舟云学术

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Phase equilibria modelling constraints on P–T conditions during fluid catalysed conversion of granulite to eclogite in the Bergen Arcs, Norway

Published:2017-12-20 Issue:3 Volume:36 Page:315-342
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J Metamorph Geol

Author:

Bhowany K.¹,Hand M.¹,Clark C.²,Kelsey D. E.¹,Reddy S. M.²^ORCID,Pearce M. A.³^ORCID,Tucker N. M.¹,Morrissey L. J.⁴

Affiliation:

1. Department of Earth Sciences School of Physical Sciences University of Adelaide Adelaide SA Australia

2. Department of Applied Geology Curtin University Perth WA Australia

3. CSIRO Mineral Resources Australian Resources Research Centre Perth WA Australia

4. School of National and Built Environments University of South Australia Adelaide SA Australia

Funder

Australian Research Council

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12294

Reference88 articles.

1. Fluid inclusions in granulites and eclogites from the Bergen Arcs, Caledonides of W. Norway

2. Fluid-induced retrogression of granulites in the Bergen Arcs, Caledonides of W. Norway: Fluid inclusion evidence from amphibolite-facies shear zones

3. Mineral-fluid-melt interactions in high-pressure shear zones in the Bergen Arcs nappe complex, Caledonides of W. Norway: Implications for the fluid regime in Caledonian eclogite-facies metamorphism

4. High-pressure granulites at the dawn of the Proterozoic

5. Eclogitization of lower crustal granulites by fluid migration through shear zones

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