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

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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.

Original language	English
Pages (from-to)	181-184
Number of pages	4
Journal	Geophysical Research Letters
Volume	13
Issue number	3
DOIs	https://doi.org/10.1029/GL013i003p00181
Publication status	Published - Mar 1986
Externally published	Yes

All Science Journal Classification (ASJC) codes

Geophysics
General Earth and Planetary Sciences

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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.",

number = "3",

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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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DO - 10.1029/GL013i003p00181

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JO - Geophysical Research Letters

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

Abstract

All Science Journal Classification (ASJC) codes

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