Post-spinel transition in Mg2SiO4 determined by high P–T in situ X-ray diffractometry

By T. Katsura, Hitoshi Yamada, T. Shinmei, A. Kubo, Shigeaki Ono, M. Kanzaki, A. Yoneda, M. Walter, E. Ito, S. Urakawa and 2 more. 2003

227 citations recorded by the source corpus.

Subfields: Geophysics

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Modeling the Dynamics of Subducting Slabs (2008, background): “…experimental values of γ660 ≥ −6 MPa/K to γ660 = −0.5 to −3.0 MPa/K for more recent experiments, which are better able to constrain the pressure of the phase transition at different temperatures (Ito & Takahashi 1989, Irifune et al. 1998, Katsura et al. 2003, Fei et al. 2004, Litasov et al. 2005).”
Stagnant slab : A review (2009, background): “The recent measurements, however, give in general a more gentle slope ranging from -2 to -0.5 MPa/K (-2.0 MPa/K by Bina and Helffrich (1994), -0.4~-2.0 MPa/K by Katsura et al. (2003) and -1.3 MPa/K by Fei et al. (2004).”