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

Research output: Contribution to journalArticle

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). -Authors

Original languageEnglish
Pages (from-to)2457-2460
Number of pages4
JournalGeophysical Research Letters
Volume17
Issue number13
Publication statusPublished - 1990
Externally publishedYes

Fingerprint

transition element
spinel
partitioning
transition metals
analogs

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)

Cite this

Stability of (Mg,Fe)14Si5O24 at 17 GPa and 1800°C and its partitioning behavior of transition elements. / Urakawa, Satoru; Kato, M.

In: Geophysical Research Letters, Vol. 17, No. 13, 1990, p. 2457-2460.

Research output: Contribution to journalArticle

@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). -Authors",
author = "Satoru Urakawa and M. Kato",
year = "1990",
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, M.

PY - 1990

Y1 - 1990

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). -Authors

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). -Authors

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

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

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 -