Sound velocity of CaSiO3 perovskite suggests the presence of basaltic crust in the Earth’s lower mantle
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/s41586-018-0816-5.pdf
Reference51 articles.
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2. Hirose, K. & Fei, Y. Subsolidus and melting phase relations of basaltic composition in the uppermostlower mantle. Geochim. Cosmochim. Acta 66, 2099–2108 (2002).
3. Stixrude, L., Lithgow-Bertelloni, C., Kiefer, B. & Fumagalli, P. Phase stability and shear softening in CaSiO3 perovskite at high pressure. Phys. Rev. B 75, 024108 (2007).
4. Tsuchiya, T. Elasticity of subducted basaltic crust at the lower mantle pressures: Insights on the nature of deep mantle heterogeneity. Phys. Earth Planet. Inter. 188, 142–149 (2011).
5. Schmandt, B., Jacobsen, S. D., Becker, T. W. & Liu, Z. Dehydration melting at the top of the lower mantle. Science 344, 1265–1268 (2014).
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