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even identified (e.g., Hirth and Kohlstedt, 1996;
Bercovici and Karato, 2003; Ohtani et al., 2004; Hirschmann, 2006; Olson,
2010).
Throughout Earth's historical past chemical differentiation has produced continental and oceanic crust, much of which has been subducted or delaminated, producing compositional and isotopic mantle heterogeneity. Making progress has required parallel maturation of a suite of disciplines that carry key info to gentle: seismology to picture elastic and anelastic properties and material heterogeneity all through the interior, mineral physics to characterize thermo-elastic properties, phase equilibria, electronic transitions, and transport properties of Earth supplies over the full
Throughout Earth's historical past chemical differentiation has produced continental and oceanic crust, much of which has been subducted or delaminated, producing compositional and isotopic mantle heterogeneity. Making progress has required parallel maturation of a suite of disciplines that carry key info to gentle: seismology to picture elastic and anelastic properties and material heterogeneity all through the interior, mineral physics to characterize thermo-elastic properties, phase equilibria, electronic transitions, and transport properties of Earth supplies over the full
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