NOTE ON THE GEOLOGY OF THE PROTEROZOIC RAYNER COMPLEX AT MT. VECHERNYAYA NEAR MOLODEZHNAYA STATION, ENDERBY LAND
P(論文) Geological reconnaissance of the Proterozoic Rayner Complex was carried out at Mt. Vechernyaya in western Enderby Land during the 29th Japanese Antarctic Research Expedition (JARE-29,1987-1988) from February 14th to 17th, 1988. Mt. Vechernyaya (272m above sea level), situated on the coast of A...
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Language: | English |
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National Institute of Polar Research
1989
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Online Access: | https://nipr.repo.nii.ac.jp/record/2601/files/KJ00002368191.pdf https://doi.org/10.15094/00002601 https://nipr.repo.nii.ac.jp/records/2601 |
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author | マキモト, ヒロシ アサミ, マサオ / MAKIMOTO, Hiroshi ASAMI, Masao GREW, Edward S. |
author_facet | マキモト, ヒロシ アサミ, マサオ / MAKIMOTO, Hiroshi ASAMI, Masao GREW, Edward S. |
author_sort | マキモト, ヒロシ |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) Geological reconnaissance of the Proterozoic Rayner Complex was carried out at Mt. Vechernyaya in western Enderby Land during the 29th Japanese Antarctic Research Expedition (JARE-29,1987-1988) from February 14th to 17th, 1988. Mt. Vechernyaya (272m above sea level), situated on the coast of Alasheyev Bight, is about 10km east of Molodezhnaya Station.The basement around Mt. Vechernyaya consists mainly of granulite-facies, locally migmatitic, well-layered gneisses and charnockitic gneiss. The well-layered gneisses include garnet-biotite gneiss, clinopyroxene gneiss, hornblende gneiss and quartzo-feldspathic gneiss. Gneissosity trends E-W to ESE-WNW, and dips steeply to the north. Lineations, due to the preferred orientation of the mafic minerals, dip 5 to 20°east. Typical mineral assemblages of the garnet-biotite gneiss are Bi-Gt, Bi-Gt-Sil, Bi-Gt-Sil-Crd and Bi-Gt-Opx-Mt. The above cordierite-bearing assemblage is the third report from the Molodezhnaya area. Six well-layered gneisses were sampled for geochronological studies. The charnockitic gneiss, which is exposed in an elongate body, has mineral lineations but no marked compositional layering. Its intrusive relation with the well-layered gneisses suggests an igneous origin. This rock consists mainly of quartz, K-feldspar and plagioclase with minor orthopyroxene, clinopyroxene, hornblende and biotite.Granite and pegmatite dikes, a few centimeters to 1m thick, intrude the metamorphic rocks and charnockitic gneiss throughout the area. departmental bulletin paper |
genre | Alasheyev Bight Antarc* Antarctic Enderby Land |
genre_facet | Alasheyev Bight Antarc* Antarctic Enderby Land |
geographic | Antarctic Rayner Molodezhnaya Molodezhnaya Station Vechernyaya Alasheyev Bight |
geographic_facet | Antarctic Rayner Molodezhnaya Molodezhnaya Station Vechernyaya Alasheyev Bight |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00002601 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-45.166,-45.166,-60.650,-60.650) ENVELOPE(45.850,45.850,-67.667,-67.667) ENVELOPE(46.134,46.134,-67.683,-67.683) ENVELOPE(152.171,152.171,63.127,63.127) ENVELOPE(45.667,45.667,-67.500,-67.500) |
op_collection_id | ftnipr |
op_doi | https://doi.org/10.15094/00002601 |
op_relation | Proceedings of the NIPR Symposium on Antarctic Geosciences 3 148 AA1072335X https://nipr.repo.nii.ac.jp/record/2601/files/KJ00002368191.pdf https://doi.org/10.15094/00002601 https://nipr.repo.nii.ac.jp/records/2601 |
publishDate | 1989 |
publisher | National Institute of Polar Research |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00002601 2025-04-13T14:06:10+00:00 NOTE ON THE GEOLOGY OF THE PROTEROZOIC RAYNER COMPLEX AT MT. VECHERNYAYA NEAR MOLODEZHNAYA STATION, ENDERBY LAND マキモト, ヒロシ アサミ, マサオ / MAKIMOTO, Hiroshi ASAMI, Masao GREW, Edward S. 1989-09 application/pdf https://nipr.repo.nii.ac.jp/record/2601/files/KJ00002368191.pdf https://doi.org/10.15094/00002601 https://nipr.repo.nii.ac.jp/records/2601 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Antarctic Geosciences 3 148 AA1072335X https://nipr.repo.nii.ac.jp/record/2601/files/KJ00002368191.pdf https://doi.org/10.15094/00002601 https://nipr.repo.nii.ac.jp/records/2601 1989 ftnipr https://doi.org/10.15094/00002601 2025-03-19T10:19:57Z P(論文) Geological reconnaissance of the Proterozoic Rayner Complex was carried out at Mt. Vechernyaya in western Enderby Land during the 29th Japanese Antarctic Research Expedition (JARE-29,1987-1988) from February 14th to 17th, 1988. Mt. Vechernyaya (272m above sea level), situated on the coast of Alasheyev Bight, is about 10km east of Molodezhnaya Station.The basement around Mt. Vechernyaya consists mainly of granulite-facies, locally migmatitic, well-layered gneisses and charnockitic gneiss. The well-layered gneisses include garnet-biotite gneiss, clinopyroxene gneiss, hornblende gneiss and quartzo-feldspathic gneiss. Gneissosity trends E-W to ESE-WNW, and dips steeply to the north. Lineations, due to the preferred orientation of the mafic minerals, dip 5 to 20°east. Typical mineral assemblages of the garnet-biotite gneiss are Bi-Gt, Bi-Gt-Sil, Bi-Gt-Sil-Crd and Bi-Gt-Opx-Mt. The above cordierite-bearing assemblage is the third report from the Molodezhnaya area. Six well-layered gneisses were sampled for geochronological studies. The charnockitic gneiss, which is exposed in an elongate body, has mineral lineations but no marked compositional layering. Its intrusive relation with the well-layered gneisses suggests an igneous origin. This rock consists mainly of quartz, K-feldspar and plagioclase with minor orthopyroxene, clinopyroxene, hornblende and biotite.Granite and pegmatite dikes, a few centimeters to 1m thick, intrude the metamorphic rocks and charnockitic gneiss throughout the area. departmental bulletin paper Other/Unknown Material Alasheyev Bight Antarc* Antarctic Enderby Land National Institute of Polar Research Repository, Japan Antarctic Rayner ENVELOPE(-45.166,-45.166,-60.650,-60.650) Molodezhnaya ENVELOPE(45.850,45.850,-67.667,-67.667) Molodezhnaya Station ENVELOPE(46.134,46.134,-67.683,-67.683) Vechernyaya ENVELOPE(152.171,152.171,63.127,63.127) Alasheyev Bight ENVELOPE(45.667,45.667,-67.500,-67.500) |
spellingShingle | マキモト, ヒロシ アサミ, マサオ / MAKIMOTO, Hiroshi ASAMI, Masao GREW, Edward S. NOTE ON THE GEOLOGY OF THE PROTEROZOIC RAYNER COMPLEX AT MT. VECHERNYAYA NEAR MOLODEZHNAYA STATION, ENDERBY LAND |
title | NOTE ON THE GEOLOGY OF THE PROTEROZOIC RAYNER COMPLEX AT MT. VECHERNYAYA NEAR MOLODEZHNAYA STATION, ENDERBY LAND |
title_full | NOTE ON THE GEOLOGY OF THE PROTEROZOIC RAYNER COMPLEX AT MT. VECHERNYAYA NEAR MOLODEZHNAYA STATION, ENDERBY LAND |
title_fullStr | NOTE ON THE GEOLOGY OF THE PROTEROZOIC RAYNER COMPLEX AT MT. VECHERNYAYA NEAR MOLODEZHNAYA STATION, ENDERBY LAND |
title_full_unstemmed | NOTE ON THE GEOLOGY OF THE PROTEROZOIC RAYNER COMPLEX AT MT. VECHERNYAYA NEAR MOLODEZHNAYA STATION, ENDERBY LAND |
title_short | NOTE ON THE GEOLOGY OF THE PROTEROZOIC RAYNER COMPLEX AT MT. VECHERNYAYA NEAR MOLODEZHNAYA STATION, ENDERBY LAND |
title_sort | note on the geology of the proterozoic rayner complex at mt. vechernyaya near molodezhnaya station, enderby land |
url | https://nipr.repo.nii.ac.jp/record/2601/files/KJ00002368191.pdf https://doi.org/10.15094/00002601 https://nipr.repo.nii.ac.jp/records/2601 |