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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Language: | English |
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National Institute of Polar Research
2001
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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 |
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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 |