POSTSPINEL TRANSFORMATIONS AND THE WIDTH OF THE 670-KM DISCONTINUITY - A COMMENT ON POSTSPINEL TRANSFORMATIONS IN THE SYSTEM MG2SIO4-FE2SIO4 AND SOME GEOPHYSICAL IMPLICATIONS BY ITO,E. AND TAKAHASHI,E.

Eitemau Tebyg

• Postspinel transformations and the width of the 670-km discontinuity: a comment on "Postspinel transformations in the system Mg2SiO4-Fe2SiO4 and some geophysical implications' by E. Ito and E. Takahashi
  gan: Wood, B
  Cyhoeddwyd: (1990)
• Expanding the Ambient-Pressure Phase Space of CaFe2O4‑Type Sodium Postspinel Host–Guest Compounds
  gan: Justin C. Hancock, et al.
  Cyhoeddwyd: (2021-09-01)
• MANTLE GEOPHYSICS - MINERALOGICAL PHASE-CHANGE AT THE 670-KM DISCONTINUITY
  gan: Wood, B
  Cyhoeddwyd: (1989)
• Mineralogical phase change at the 670-km discontinuity
  gan: Wood, B
  Cyhoeddwyd: (1989)
• The nature of the olivine - spinel transition in the Mg2SiO4-Fe2SiO4 system and its geophysical implications.
  gan: Sung, Chien-Min, 1947-
  Cyhoeddwyd: (2010)