Carbonate polymorphism reverses carbonate-silicate reaction in Earth's lower mantle

Mingda Lv(Argonne National Laboratory), Vitali B. Prakapenka(Primary Source), James Badro(Centre National de la Recherche Scientifique), Susannah M. Dorfman(École Polytechnique Fédérale de Lausanne), Eran Greenberg(University of Chicago), Stephan Borensztajn(Institut de physique du globe de Paris)
AGU Fall Meeting Abstracts
December 1, 2018
Cited by 0

Related Papers

Iron Partitioning in Earth's Mantle: Toward a Deep Lower Mantle Discontinuity
|Science|2003|526
Synthesis and characterization of a binary noble metal nitride
|Nature Materials|2004|526
Electronic Transitions in Perovskite: Possible Nonconvecting Layers in the Lower Mantle
|Science|2004|372
A seismologically consistent compositional model of Earth’s core
|Proceedings of the National Academy of Sciences|2014|333
X-ray Imaging of Stress and Strain of Diamond, Iron, and Tungsten at Megabar Pressures
|Science|1997|257