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High‐grade metamorphism and partial melting of basic and intermediate rocks

Abstract:

Rocks of basic and intermediate bulk composition occur in orogenic terranes from all geological time periods and are thought to represent significant petrological components of the middle and lower continental crust. However, the former lack of appropriate thermodynamic models for silicate melt, amphibole and clinopyroxene that can be applied to such lithologies at high temperature has inhibited effective phase equilibrium modelling of their petrological evolution during amphibolite- and gran...

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1111/jmg.12212

Authors


More by this author
Institution:
University of Oxford
Division:
MPLS Division
Department:
Earth Sciences
Oxford college:
St Cross College
Role:
Author
ORCID:
0000-0002-6959-0462
More by this author
Role:
Author
ORCID:
0000-0001-6024-6457
Publisher:
Wiley Publisher's website
Journal:
Journal of Metamorphic Geology
Volume:
34
Issue:
9
Pages:
871-892
Publication date:
2016-08-12
Acceptance date:
2016-07-01
DOI:
EISSN:
1525-1314
ISSN:
0263-4929
Language:
English
Keywords:
Pubs id:
pubs:932895
UUID:
uuid:d82f1b80-0c6c-46da-bdee-e3633a74e1d5
Local pid:
pubs:932895
Source identifiers:
932895
Deposit date:
2020-01-10

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