Ultrahigh temperature sapphirine-osumilite and sapphirine-quartz granulites from Bunt Island in the Napier Complex, East Antarctica -Reconnaissance estimation of P-T evolution -

P(論文) The summer party of the 39th Japanese Antarctic Research Expedition (1997-1998) carried out geological field work on Bunt Island at the southeastern end of Amundsen Bay, Enderby Land, which is in the highest-grade metamorphic region in the Napier Complex. The island is underlain by various kin...

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Main Authors: Osanai, Yasuhito, Toyoshima, Tsuyoshi, Owada, Masaaki, Tsunogae, Toshiaki, Hokada, Tomokazu, Crowe, Warwick A., Kusachi, Isao
Language:English
Published: National Institute of Polar Research 2001
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3082/files/KJ00000044200.pdf
https://doi.org/10.15094/00003082
https://nipr.repo.nii.ac.jp/records/3082
_version_ 1829303253771223040
author Osanai, Yasuhito
Toyoshima, Tsuyoshi
Owada, Masaaki
Tsunogae, Toshiaki
Hokada, Tomokazu
Crowe, Warwick A.
Kusachi, Isao
author_facet Osanai, Yasuhito
Toyoshima, Tsuyoshi
Owada, Masaaki
Tsunogae, Toshiaki
Hokada, Tomokazu
Crowe, Warwick A.
Kusachi, Isao
author_sort Osanai, Yasuhito
collection National Institute of Polar Research Repository, Japan
description P(論文) The summer party of the 39th Japanese Antarctic Research Expedition (1997-1998) carried out geological field work on Bunt Island at the southeastern end of Amundsen Bay, Enderby Land, which is in the highest-grade metamorphic region in the Napier Complex. The island is underlain by various kinds of ultrahigh-temperature (UHT) metamorphic rocks including osumilite-bearing aluminous sapphirine-garnet-orthopyroxene granulite and quartz-predominant sapphirine-garnet-sillimanite gneiss containing the assemblage sapphirine-quartz. Osumilite-bearing aluminous granulite is silica-undersaturated, aluminous and magnesian chromium-rich chemical affinity. Osumilite-bearing granulite from Bunt Island could be formed through the mixing of clayey materials or other felsic components derived from felsic igneous rocks with a relatively high proportion of mafic to ultramafic detritus in the sedimentary precursor. The chemical mixing could have taken place during c. 3.2 and c. 2.5 Ga. P-T estimation for osumilite-bearing granulite and related sapphirine-quartz gneiss indicates ultrahigh-temperature condition (~1100℃, ~1100 Mpa) as well as other high-grade rocks from the Napier Complex, but the rocks from Bunt Island clearly show isothermal decompression in part of the clockwise P-T evolutional process. departmental bulletin paper
genre Amundsen Bay
Antarc*
Antarctic
Antarctica
Bunt Island
East Antarctica
Enderby Land
Polar geoscience
genre_facet Amundsen Bay
Antarc*
Antarctic
Antarctica
Bunt Island
East Antarctica
Enderby Land
Polar geoscience
geographic Antarctic
East Antarctica
Napier
Bunt
Amundsen Bay
Bunt Island
geographic_facet Antarctic
East Antarctica
Napier
Bunt
Amundsen Bay
Bunt Island
id ftnipr:oai:nipr.repo.nii.ac.jp:00003082
institution Open Polar
language English
long_lat ENVELOPE(-58.440,-58.440,-62.167,-62.167)
ENVELOPE(66.367,66.367,-70.767,-70.767)
ENVELOPE(50.000,50.000,-66.917,-66.917)
ENVELOPE(50.950,50.950,-67.150,-67.150)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003082
op_relation Polar geoscience
14
1
24
AA1130866X
https://nipr.repo.nii.ac.jp/record/3082/files/KJ00000044200.pdf
https://doi.org/10.15094/00003082
https://nipr.repo.nii.ac.jp/records/3082
publishDate 2001
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003082 2025-04-13T14:06:44+00:00 Ultrahigh temperature sapphirine-osumilite and sapphirine-quartz granulites from Bunt Island in the Napier Complex, East Antarctica -Reconnaissance estimation of P-T evolution - Osanai, Yasuhito Toyoshima, Tsuyoshi Owada, Masaaki Tsunogae, Toshiaki Hokada, Tomokazu Crowe, Warwick A. Kusachi, Isao 2001-10 application/pdf https://nipr.repo.nii.ac.jp/record/3082/files/KJ00000044200.pdf https://doi.org/10.15094/00003082 https://nipr.repo.nii.ac.jp/records/3082 eng eng National Institute of Polar Research Polar geoscience 14 1 24 AA1130866X https://nipr.repo.nii.ac.jp/record/3082/files/KJ00000044200.pdf https://doi.org/10.15094/00003082 https://nipr.repo.nii.ac.jp/records/3082 sapphirine osumilite P-T path Bunt Island Napier Complex 2001 ftnipr https://doi.org/10.15094/00003082 2025-03-19T10:19:57Z P(論文) The summer party of the 39th Japanese Antarctic Research Expedition (1997-1998) carried out geological field work on Bunt Island at the southeastern end of Amundsen Bay, Enderby Land, which is in the highest-grade metamorphic region in the Napier Complex. The island is underlain by various kinds of ultrahigh-temperature (UHT) metamorphic rocks including osumilite-bearing aluminous sapphirine-garnet-orthopyroxene granulite and quartz-predominant sapphirine-garnet-sillimanite gneiss containing the assemblage sapphirine-quartz. Osumilite-bearing aluminous granulite is silica-undersaturated, aluminous and magnesian chromium-rich chemical affinity. Osumilite-bearing granulite from Bunt Island could be formed through the mixing of clayey materials or other felsic components derived from felsic igneous rocks with a relatively high proportion of mafic to ultramafic detritus in the sedimentary precursor. The chemical mixing could have taken place during c. 3.2 and c. 2.5 Ga. P-T estimation for osumilite-bearing granulite and related sapphirine-quartz gneiss indicates ultrahigh-temperature condition (~1100℃, ~1100 Mpa) as well as other high-grade rocks from the Napier Complex, but the rocks from Bunt Island clearly show isothermal decompression in part of the clockwise P-T evolutional process. departmental bulletin paper Other/Unknown Material Amundsen Bay Antarc* Antarctic Antarctica Bunt Island East Antarctica Enderby Land Polar geoscience National Institute of Polar Research Repository, Japan Antarctic East Antarctica Napier ENVELOPE(-58.440,-58.440,-62.167,-62.167) Bunt ENVELOPE(66.367,66.367,-70.767,-70.767) Amundsen Bay ENVELOPE(50.000,50.000,-66.917,-66.917) Bunt Island ENVELOPE(50.950,50.950,-67.150,-67.150)
spellingShingle sapphirine
osumilite
P-T path
Bunt Island
Napier Complex
Osanai, Yasuhito
Toyoshima, Tsuyoshi
Owada, Masaaki
Tsunogae, Toshiaki
Hokada, Tomokazu
Crowe, Warwick A.
Kusachi, Isao
Ultrahigh temperature sapphirine-osumilite and sapphirine-quartz granulites from Bunt Island in the Napier Complex, East Antarctica -Reconnaissance estimation of P-T evolution -
title Ultrahigh temperature sapphirine-osumilite and sapphirine-quartz granulites from Bunt Island in the Napier Complex, East Antarctica -Reconnaissance estimation of P-T evolution -
title_full Ultrahigh temperature sapphirine-osumilite and sapphirine-quartz granulites from Bunt Island in the Napier Complex, East Antarctica -Reconnaissance estimation of P-T evolution -
title_fullStr Ultrahigh temperature sapphirine-osumilite and sapphirine-quartz granulites from Bunt Island in the Napier Complex, East Antarctica -Reconnaissance estimation of P-T evolution -
title_full_unstemmed Ultrahigh temperature sapphirine-osumilite and sapphirine-quartz granulites from Bunt Island in the Napier Complex, East Antarctica -Reconnaissance estimation of P-T evolution -
title_short Ultrahigh temperature sapphirine-osumilite and sapphirine-quartz granulites from Bunt Island in the Napier Complex, East Antarctica -Reconnaissance estimation of P-T evolution -
title_sort ultrahigh temperature sapphirine-osumilite and sapphirine-quartz granulites from bunt island in the napier complex, east antarctica -reconnaissance estimation of p-t evolution -
topic sapphirine
osumilite
P-T path
Bunt Island
Napier Complex
topic_facet sapphirine
osumilite
P-T path
Bunt Island
Napier Complex
url https://nipr.repo.nii.ac.jp/record/3082/files/KJ00000044200.pdf
https://doi.org/10.15094/00003082
https://nipr.repo.nii.ac.jp/records/3082