Complex, Multilayered Azimuthal Anisotropy Beneath Tibet: Evidence for Co-Existing Channel Flow and Pure-Shear Crustal Thickening
Geophysical Journal International - United Kingdom
doi 10.1093/gji/ggx266
Full Text
Open PDFAbstract
Available in full text
Date
June 20, 2017
Authors
Publisher
Oxford University Press (OUP)