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.
1. autor: | Wood, B |
---|---|
Format: | Journal article |
Wydane: |
1990
|
Podobne zapisy
-
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
od: Wood, B
Wydane: (1990) -
Expanding the Ambient-Pressure Phase Space of CaFe2O4‑Type Sodium Postspinel Host–Guest Compounds
od: Justin C. Hancock, i wsp.
Wydane: (2021-09-01) -
MANTLE GEOPHYSICS - MINERALOGICAL PHASE-CHANGE AT THE 670-KM DISCONTINUITY
od: Wood, B
Wydane: (1989) -
Mineralogical phase change at the 670-km discontinuity
od: Wood, B
Wydane: (1989) -
The nature of the olivine - spinel transition in the Mg2SiO4-Fe2SiO4 system and its geophysical implications.
od: Sung, Chien-Min, 1947-
Wydane: (2010)