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Butler, Jared P., Beaumont, Christopher (2017) Subduction zone decoupling/retreat modeling explains south Tibet (Xigaze) and other supra-subduction zone ophiolites and their UHP mineral phases. Earth and Planetary Science Letters, 463. 101-117 doi:10.1016/j.epsl.2017.01.025

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Reference TypeJournal (article/letter/editorial)
TitleSubduction zone decoupling/retreat modeling explains south Tibet (Xigaze) and other supra-subduction zone ophiolites and their UHP mineral phases
JournalEarth and Planetary Science Letters
AuthorsButler, Jared P.Author
Beaumont, ChristopherAuthor
Year2017 (April)Volume463
PublisherElsevier BV
DOIdoi:10.1016/j.epsl.2017.01.025Search in ResearchGate
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Mindat Ref. ID391279Long-form Identifiermindat:1:5:391279:3
GUID0
Full ReferenceButler, Jared P., Beaumont, Christopher (2017) Subduction zone decoupling/retreat modeling explains south Tibet (Xigaze) and other supra-subduction zone ophiolites and their UHP mineral phases. Earth and Planetary Science Letters, 463. 101-117 doi:10.1016/j.epsl.2017.01.025
Plain TextButler, Jared P., Beaumont, Christopher (2017) Subduction zone decoupling/retreat modeling explains south Tibet (Xigaze) and other supra-subduction zone ophiolites and their UHP mineral phases. Earth and Planetary Science Letters, 463. 101-117 doi:10.1016/j.epsl.2017.01.025
In(2017) Earth and Planetary Science Letters Vol. 463. Elsevier BV


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