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The lower crust of the Gangdese magmatic arc, southern Tibet, implication for the growth of continental crust

Abstract:

Magmatic arcs are thought to be the primary sites of modern-day continental crustal growth, and arc crustal sections provide an exceptional opportunity to directly observe the geological processes that occur there, yet few deeply exposed arc sections are available for direct study. The Gangdese magmatic arc, southern Tibet, formed during the Mesozoic subduction of Neo-Tethyan oceanic lithosphere and Cenozoic collision between the Indian and Asian continents, and represent juvenile continental...

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1016/j.gr.2019.07.010

Authors


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Institution:
University of Oxford
Division:
MPLS Division
Department:
Earth Sciences
Oxford college:
St Cross College
Role:
Author
ORCID:
0000-0002-6959-0462
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Publisher:
Elsevier Publisher's website
Journal:
Gondwana Research
Volume:
77
Pages:
136-146
Publication date:
2019-08-26
Acceptance date:
2019-07-30
DOI:
EISSN:
1878-0571
ISSN:
1342-937X
Source identifiers:
1081643
Keywords:
Pubs id:
pubs:1081643
UUID:
uuid:3d341539-8205-452b-bfa5-b84a7f57c8a6
Local pid:
pubs:1081643
Deposit date:
2020-01-10

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