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Crustal melting, ductile flow, and deformation in mountain belts: Cause and effect relationships

Abstract:

Exhumed sections of migmatites are beautifully exposed in the middle crust of old orogens such as the Proterozoic Wet Mountains of Colorado and young Tertiary-active orogens such as the Himalaya and Karakoram. Migmatites and leucogranites occur both on a regional scale (e.g., Greater Himalayan Sequence) and along more restricted shear zones and strike-slip faults (e.g., Karakoram, Jiale, and Red River faults). Melting and deformation are clearly diachronous across orogenic belts over space an...

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Publication status:
Published

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Publisher copy:
10.1130/RF.L006.1

Authors


Journal:
LITHOSPHERE
Volume:
5
Issue:
6
Pages:
547-554
Publication date:
2013-12-01
DOI:
EISSN:
1947-4253
ISSN:
1941-8264
Language:
English
Pubs id:
pubs:443569
UUID:
uuid:03ad0c2d-412e-4090-89e3-c34d2325b188
Local pid:
pubs:443569
Source identifiers:
443569
Deposit date:
2014-02-14

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