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 › peer-review

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)

Access to Document

10.1029/GL017i013p02457

Cite this

@article{6e7c3186d5c0482d9d048673d130fb4c,

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

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",

month = dec,

doi = "10.1029/GL017i013p02457",

language = "English",

volume = "17",

pages = "2457--2460",

journal = "Geophysical Research Letters",

issn = "0094-8276",

publisher = "American Geophysical Union",

number = "13",

}

TY - JOUR

T1 - Stability of (Mg,Fe)14Si5O24 AT 17 GPa and 1800°C and its partitioning behavior of transition elements

AU - Urakawa, Satoru

AU - Kato, Manabu

PY - 1990/12

Y1 - 1990/12

N2 - 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).

AB - 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).

UR - http://www.scopus.com/inward/record.url?scp=0025625814&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0025625814&partnerID=8YFLogxK

U2 - 10.1029/GL017i013p02457

DO - 10.1029/GL017i013p02457

M3 - Article

AN - SCOPUS:0025625814

VL - 17

SP - 2457

EP - 2460

JO - Geophysical Research Letters

JF - Geophysical Research Letters

SN - 0094-8276

IS - 13

ER -

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

Abstract

ASJC Scopus subject areas

Access to Document

Other files and links

Fingerprint

Cite this