Melting experiment on natural lherzolite at 20 GPa: Formation of phase B coexisting with garnet

Takumi Kato; Mineo Kumazawa

doi:10.1029/GL013i003p00181

Melting experiment on natural lherzolite at 20 GPa: Formation of phase B coexisting with garnet

Takumi Kato
, Mineo Kumazawa

研究成果: ジャーナルへの寄稿 › 学術誌 › 査読

18 被引用数 (Scopus)

抄録

A melting experiment has been made on a natural lherzolite (spinel lherzolite, KLB‐1) at 20 GPa and 2160°C under hydrous conditions. The stable phase assemblage is liquid, garnet, and modified spinel, which is replaced by phase B above the melting temperature of modified spinel, and garnet is the liquidus phase at this pressure.

本文言語	英語
ページ（範囲）	181-184
ページ数	4
ジャーナル	Geophysical Research Letters
巻	13
号	3
DOI	https://doi.org/10.1029/GL013i003p00181
出版ステータス	出版済み - 3月 1986
外部発表	はい

!!!All Science Journal Classification (ASJC) codes

地球物理学
地球惑星科学一般

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10.1029/GL013i003p00181

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title = "Melting experiment on natural lherzolite at 20 GPa: Formation of phase B coexisting with garnet",

abstract = "A melting experiment has been made on a natural lherzolite (spinel lherzolite, KLB‐1) at 20 GPa and 2160°C under hydrous conditions. The stable phase assemblage is liquid, garnet, and modified spinel, which is replaced by phase B above the melting temperature of modified spinel, and garnet is the liquidus phase at this pressure.",

author = "Takumi Kato and Mineo Kumazawa",

year = "1986",

month = mar,

doi = "10.1029/GL013i003p00181",

language = "English",

volume = "13",

pages = "181--184",

journal = "Geophysical Research Letters",

issn = "0094-8276",

publisher = "John Wiley and Sons Inc.",

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T1 - Melting experiment on natural lherzolite at 20 GPa

T2 - Formation of phase B coexisting with garnet

AU - Kato, Takumi

AU - Kumazawa, Mineo

PY - 1986/3

Y1 - 1986/3

N2 - A melting experiment has been made on a natural lherzolite (spinel lherzolite, KLB‐1) at 20 GPa and 2160°C under hydrous conditions. The stable phase assemblage is liquid, garnet, and modified spinel, which is replaced by phase B above the melting temperature of modified spinel, and garnet is the liquidus phase at this pressure.

AB - A melting experiment has been made on a natural lherzolite (spinel lherzolite, KLB‐1) at 20 GPa and 2160°C under hydrous conditions. The stable phase assemblage is liquid, garnet, and modified spinel, which is replaced by phase B above the melting temperature of modified spinel, and garnet is the liquidus phase at this pressure.

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UR - https://www.scopus.com/pages/publications/0022672827#tab=citedBy

U2 - 10.1029/GL013i003p00181

DO - 10.1029/GL013i003p00181

M3 - Article

AN - SCOPUS:0022672827

SN - 0094-8276

VL - 13

SP - 181

EP - 184

JO - Geophysical Research Letters

JF - Geophysical Research Letters

IS - 3

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Melting experiment on natural lherzolite at 20 GPa: Formation of phase B coexisting with garnet

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!!!All Science Journal Classification (ASJC) codes

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