Article ID Journal Published Year Pages File Type
4731301 Journal of Asian Earth Sciences 2013 10 Pages PDF
Abstract
► The 410 and 660 interfaces beneath east Tibet are investigated. ► Both interfaces beneath LMS are depressed. ► The depressions are from a sinking dry mantle flow. ► The sinking flow is from eastward asthenosphere resisted by Yangtze Craton.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Preview
Seismic signature of the mantle transition zone beneath eastern Tibet and Sichuan Basin
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