MINERAL PARAGENESIS OF THE SAPPHIRINE-BEARING ROCK FROM THE AUSTKAMPANE AREA OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA

P(論文) A sapphirine-bearing rock occurs in the Austkampane area of the Sør Rondane Mountains, East Antarctica, where sillimanite-garnet-biotite gneisses of the granulite facies are widespread. The constituent minerals of the rock include sapphirine, phlogopite, hydrous cordierite, plagioclase, gedrit...

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Main Authors: イシズカ, ヒデオ, スズキ, サトコ, コジマ, ヒデヤス, ISHIZUKA, Hideo, SUZUKI, Satoko, KOJIMA, Hideyasu
Language:English
Published: National Institute of Polar Research 1995
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/2786/files/KJ00002368416.pdf
https://doi.org/10.15094/00002786
https://nipr.repo.nii.ac.jp/records/2786
_version_ 1829312625674027008
author イシズカ, ヒデオ
スズキ, サトコ
コジマ, ヒデヤス
ISHIZUKA, Hideo
SUZUKI, Satoko
KOJIMA, Hideyasu
author_facet イシズカ, ヒデオ
スズキ, サトコ
コジマ, ヒデヤス
ISHIZUKA, Hideo
SUZUKI, Satoko
KOJIMA, Hideyasu
author_sort イシズカ, ヒデオ
collection National Institute of Polar Research Repository, Japan
description P(論文) A sapphirine-bearing rock occurs in the Austkampane area of the Sør Rondane Mountains, East Antarctica, where sillimanite-garnet-biotite gneisses of the granulite facies are widespread. The constituent minerals of the rock include sapphirine, phlogopite, hydrous cordierite, plagioclase, gedrite, orthopyroxene, spinel, corundum, rutile and ilmenite. The bulk rock analyses show basaltic compositions in a broad sense, but in a strict sense they are enriched in Al_2O_3,MgO, Cr and Ni, suggesting a precursor with troctolitic composition. Among the constituent minerals, it is most characteristic that the sapphirine is never in direct contact with orthopyroxene, and between the two phases occur the hydrous cordierite-spinel symplectite. This indicates that the reaction sapphirine+orthopyroxene+H_2O=hydrous cordierite+spinel may have occurred. In the system MgO-Al_2O_3-SiO_2-H_2O, this reaction is pressure sensitive with a very shallow and negative dP/dT slope at about 4kbar on the P-T diagram. Geothermometers, including sapphirine-spinel, cordierite-spinel, and Al_2O_3 content at the Ml-site of orthopyroxene, yield around 820-870℃ for the assemblage prior to the reaction, and about 770℃ for the assemblage after the reaction. It follows that the sapphirine-bearing rock may have suffered nearly isothermal decompression after its peak metamorphism. Such a decompression has recently been reported from other terrains of East Antarctica, suggesting the geological episode common in these terrains. departmental bulletin paper
genre Antarc*
Antarctica
East Antarctica
genre_facet Antarc*
Antarctica
East Antarctica
geographic East Antarctica
Sør-Rondane
Sør Rondane Mountains
Austkampane
geographic_facet East Antarctica
Sør-Rondane
Sør Rondane Mountains
Austkampane
id ftnipr:oai:nipr.repo.nii.ac.jp:00002786
institution Open Polar
language English
long_lat ENVELOPE(25.000,25.000,-72.000,-72.000)
ENVELOPE(25.000,25.000,-72.000,-72.000)
ENVELOPE(25.250,25.250,-71.800,-71.800)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00002786
op_relation Proceedings of the NIPR Symposium on Antarctic Geosciences
8
65
74
AA1072335X
https://nipr.repo.nii.ac.jp/record/2786/files/KJ00002368416.pdf
https://doi.org/10.15094/00002786
https://nipr.repo.nii.ac.jp/records/2786
publishDate 1995
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00002786 2025-04-13T14:08:24+00:00 MINERAL PARAGENESIS OF THE SAPPHIRINE-BEARING ROCK FROM THE AUSTKAMPANE AREA OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA イシズカ, ヒデオ スズキ, サトコ コジマ, ヒデヤス ISHIZUKA, Hideo SUZUKI, Satoko KOJIMA, Hideyasu 1995-09 application/pdf https://nipr.repo.nii.ac.jp/record/2786/files/KJ00002368416.pdf https://doi.org/10.15094/00002786 https://nipr.repo.nii.ac.jp/records/2786 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Antarctic Geosciences 8 65 74 AA1072335X https://nipr.repo.nii.ac.jp/record/2786/files/KJ00002368416.pdf https://doi.org/10.15094/00002786 https://nipr.repo.nii.ac.jp/records/2786 1995 ftnipr https://doi.org/10.15094/00002786 2025-03-19T10:19:57Z P(論文) A sapphirine-bearing rock occurs in the Austkampane area of the Sør Rondane Mountains, East Antarctica, where sillimanite-garnet-biotite gneisses of the granulite facies are widespread. The constituent minerals of the rock include sapphirine, phlogopite, hydrous cordierite, plagioclase, gedrite, orthopyroxene, spinel, corundum, rutile and ilmenite. The bulk rock analyses show basaltic compositions in a broad sense, but in a strict sense they are enriched in Al_2O_3,MgO, Cr and Ni, suggesting a precursor with troctolitic composition. Among the constituent minerals, it is most characteristic that the sapphirine is never in direct contact with orthopyroxene, and between the two phases occur the hydrous cordierite-spinel symplectite. This indicates that the reaction sapphirine+orthopyroxene+H_2O=hydrous cordierite+spinel may have occurred. In the system MgO-Al_2O_3-SiO_2-H_2O, this reaction is pressure sensitive with a very shallow and negative dP/dT slope at about 4kbar on the P-T diagram. Geothermometers, including sapphirine-spinel, cordierite-spinel, and Al_2O_3 content at the Ml-site of orthopyroxene, yield around 820-870℃ for the assemblage prior to the reaction, and about 770℃ for the assemblage after the reaction. It follows that the sapphirine-bearing rock may have suffered nearly isothermal decompression after its peak metamorphism. Such a decompression has recently been reported from other terrains of East Antarctica, suggesting the geological episode common in these terrains. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica National Institute of Polar Research Repository, Japan East Antarctica Sør-Rondane ENVELOPE(25.000,25.000,-72.000,-72.000) Sør Rondane Mountains ENVELOPE(25.000,25.000,-72.000,-72.000) Austkampane ENVELOPE(25.250,25.250,-71.800,-71.800)
spellingShingle イシズカ, ヒデオ
スズキ, サトコ
コジマ, ヒデヤス
ISHIZUKA, Hideo
SUZUKI, Satoko
KOJIMA, Hideyasu
MINERAL PARAGENESIS OF THE SAPPHIRINE-BEARING ROCK FROM THE AUSTKAMPANE AREA OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title MINERAL PARAGENESIS OF THE SAPPHIRINE-BEARING ROCK FROM THE AUSTKAMPANE AREA OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_full MINERAL PARAGENESIS OF THE SAPPHIRINE-BEARING ROCK FROM THE AUSTKAMPANE AREA OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_fullStr MINERAL PARAGENESIS OF THE SAPPHIRINE-BEARING ROCK FROM THE AUSTKAMPANE AREA OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_full_unstemmed MINERAL PARAGENESIS OF THE SAPPHIRINE-BEARING ROCK FROM THE AUSTKAMPANE AREA OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_short MINERAL PARAGENESIS OF THE SAPPHIRINE-BEARING ROCK FROM THE AUSTKAMPANE AREA OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_sort mineral paragenesis of the sapphirine-bearing rock from the austkampane area of the sør rondane mountains, east antarctica
url https://nipr.repo.nii.ac.jp/record/2786/files/KJ00002368416.pdf
https://doi.org/10.15094/00002786
https://nipr.repo.nii.ac.jp/records/2786