Effects of melt depletion on the density and seismic velocity of garnet and spinel lherzolite
By D. Schutt, C. Lesher. 2006
343 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/f08679eaf68c9f50a91750050b43772147e8295a
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In Geophysics
- J. A. Connolly
- J. C. Afonso
- William L Griffin
- S. O’Reilly
- A. Jones
- Yingjie Yang
- Javier Fullea
- A. Maggi
Citations in the corpus
- 3‐D multiobservable probabilistic inversion for the compositional and thermal structure of the lithosphere and upper mantle. I: a priori petrological information and geophysical observables (2013, background): “, 2008], and mineral physics methods [Schutt and Lesher, 2006] for identical compositions.”
- Integrated geophysical‐petrological modeling of the lithosphere and sublithospheric upper mantle: Methodology and applications (2008, background): “The possibility of distinguishing compositional from thermal effects using only seismic information is still unclear [e.g., Cammarano et al., 2003; Lee, 2003; Artemieva et al., 2004; Afonso et al., 2005; Faul and Jackson, 2005; Deen et al., 2006; Priestley and McKenzie, 2006; Schutt and Lesher, 2006”
- Complex subduction and small-scale convection revealed by body-wave tomography of the western United States upper mantle (2010, background): “There is no consensus as to how strongly melt depletion affects VP/VS (Lee, 2003; Schutt and Lesher, 2006).”
- Temperature, lithosphere‐asthenosphere boundary, and heat flux beneath the Antarctic Plate inferred from seismic velocities (2015, background): “…as done in forward calculations by Fullea et al. [2009]; however, the effect of composition generally yields velocity anomalies that are<1% in the shallow mantle, meaning the compositional effects are difficult to resolve from seismic tomography [Goes et al., 2000; Schutt and Lesher, 2006].”
- The relationship between shear wave velocity, temperature, attenuation and viscosity in the shallow part of the mantle (2013, background): “Though in principle V s is controlled by the composition and temperature of the mantle, a number of studies (Jordan, 1979; Schutt and Lesher, 2006; Priestley and McKenzie, 2006) have concluded that change in V s resulting from melt extraction from a garnet peridotite is small, and is unlikely to exc”