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EBSD‐based criteria for coesite‐quartz transformation

Abstract:

Ultra high pressure (UHP) metamorphism observed in continental terranes implies that continental crust can subduct to ~40 kbar before exhuming to the surface. This process is one of the least understood and widely debated parts of the orogenic cycle. The dominantly felsic composition of UHP continental terranes means that many petrology‐based techniques for determining peak pressures and temperatures are often not possible. In such cases, the detection of UHP conditions depends on the preserv...

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1111/jmg.12566

Authors


More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
ORCID:
0000-0001-7538-9418
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
ORCID:
0000-0001-9105-9953
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
Publisher:
Wiley Publisher's website
Journal:
Journal of Metamorphic Geology Journal website
Volume:
39
Issue:
2
Pages:
165-180
Publication date:
2020-09-16
Acceptance date:
2020-08-01
DOI:
ISSN:
0263-4929
Language:
English
Keywords:
Pubs id:
1123472
Local pid:
pubs:1123472
Deposit date:
2020-08-25

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