Multiple seismic reflectors in Earth's lowermost mantle

Multiple seismic reflectors in Earth's lowermost mantle

The modern view of Earth’s lowermost mantle considers a D″ region of enhanced (seismologically inferred) heterogeneity bounded by the core–mantle boundary and an interface some 150–300 km above it, with the latter often attributed to the postperovskite phase transition (in MgSiO[subscript 3]). Seism...

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Bibliographic Details
Main Authors: Shang, Xuefeng, Shim, Sang-Heon, de Hoop, Maarten, van der Hilst, Robert D
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: National Academy of Sciences (U.S.) 2014
Online Access:http://hdl.handle.net/1721.1/90329
https://orcid.org/0000-0003-1650-6818

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http://hdl.handle.net/1721.1/90329
https://orcid.org/0000-0003-1650-6818

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