Reconciling dynamic and seismic models of Earth's lower mantle: The dominant role of thermal heterogeneity

By David Rhodri Davies, S. Goes, J. Huw Davies, Bernhard S. A. Schuberth, Hans-Peter Bunge, J. Ritsema. 2012

235 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/35d7bfb0b5ac956c2ef3a7fe3a81dfc8ad4d5f3b

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In Geophysics

1. V. Lekić
2. S. Cottaar
3. J. Ritsema
4. H. V. Heijst
5. A. Deuss
6. Barbara Romanowicz
7. S. French
8. K. Priestley

Citations in the corpus

• Morphology of seismically slow lower-mantle structures (2016, background): “…provinces (Torsvik et al. 2006), major hotspots (Burke et al. 2008) and Phanerozoic kimberlites (Torsvik et al. 2010), although no statistical inference can be made about these features correlating specifically to the interior or the margin of LLSVPs (Austermann et al. 2014; Davies et al. 2015).”
• SP12RTS: a degree-12 model of shear- and compressional-wave velocity for Earth's mantle (2016, background): “…has a different composition (e.g. Su & Dziewonski 1997; Masters et al. 2000; Houser et al. 2008) or the presence of the post-perovskite (pPv) phase in the lower mantle (e.g. Iitaka et al. 2004; Murakami et al. 2004; Oganov & Ono 2004; Tsuchiya et al. 2004; Wookey et al. 2005; Davies et al. 2012).”