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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Language: | English |
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National Institute of Polar Research
1995
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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 |
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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 |