Complex, multilayered azimuthal anisotropy beneath Tibet: evidence for co-existing channel flow and pure-shear crustal thickening
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Title
Complex, multilayered azimuthal anisotropy beneath Tibet: evidence for co-existing channel flow and pure-shear crustal thickening
Authors
Keywords
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Journal
GEOPHYSICAL JOURNAL INTERNATIONAL
Volume 210, Issue 3, Pages 1823-1844
Publisher
Oxford University Press (OUP)
Online
2017-06-20
DOI
10.1093/gji/ggx266
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