Late Cenozoic Uplift of the Yulong Snow Mountain (5596m) SE Tibetan Plateau, caused by erosion and tectonic forcing.

TitleLate Cenozoic Uplift of the Yulong Snow Mountain (5596m) SE Tibetan Plateau, caused by erosion and tectonic forcing.
Publication TypeJournal Article
Year of Publication2008
AuthorsShi X, Wang E, Wang G, Fan C
JournalQuaternary Science
Volume28
Issue2
Pagination222-231