Stability of (Mg,Fe)14Si5O24 AT 17 GPa and 1800°C and its partitioning behavior of transition elements

Satoru Urakawa; Manabu Kato

doi:10.1029/GL017i013p02457

Stability of (Mg,Fe)₁₄Si₅O₂₄ AT 17 GP_a and 1800°C and its partitioning behavior of transition elements

Research output: Contribution to journal › Article

Abstract

Stability of an anhydrous analogue of phase B (AnhB) was investigated at 17 GPa and 1800°C using an MA8 type apparatus. Fe/(Mg+Fe) ratio in AnhB is restricted to within ∼0.1. The divalent transition elements such as Ni and Co are preferentially accommodated in AnhB than in modified spinel (β).

Original language	English
Pages (from-to)	2457-2460
Number of pages	4
Journal	Geophysical Research Letters
Volume	17
Issue number	13
DOIs	https://doi.org/10.1029/GL017i013p02457
Publication status	Published - Dec 1990
Externally published	Yes

ASJC Scopus subject areas

Geophysics
Earth and Planetary Sciences(all)

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Urakawa, S., & Kato, M. (1990). Stability of (Mg,Fe)₁₄Si₅O₂₄ AT 17 GP_a and 1800°C and its partitioning behavior of transition elements. Geophysical Research Letters, 17(13), 2457-2460. https://doi.org/10.1029/GL017i013p02457

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abstract = "Stability of an anhydrous analogue of phase B (AnhB) was investigated at 17 GPa and 1800°C using an MA8 type apparatus. Fe/(Mg+Fe) ratio in AnhB is restricted to within ∼0.1. The divalent transition elements such as Ni and Co are preferentially accommodated in AnhB than in modified spinel (β).",

author = "Satoru Urakawa and Manabu Kato",

year = "1990",

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