A low-velocity layer atop the mantle transition zone beneath the western Central Asian Orogenic Belt: Upper mantle melting induced by ancient slab subduction-Reference-Cited by-同舟云学术

A low-velocity layer atop the mantle transition zone beneath the western Central Asian Orogenic Belt: Upper mantle melting induced by ancient slab subduction

Published:2022-01 Issue: Volume:578 Page:117287
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Li Guohui^ORCID,Gao Yuan^ORCID,Zhou Yuanze,Ju Changhui,Shi Yutao,Cui Qinghui

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

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4. Upper mantle P velocity structure beneath the Midwestern United States derived from triplicated waveforms;Chu;Geochem. Geophys. Geosyst.,2012

5. Deep upper-mantle melting beneath the Tasman and Coral Seas detected with multiple ScS reverberations;Courtier;Earth Planet. Sci. Lett.,2007

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