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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Main Authors: マキモト, ヒロシ, アサミ, マサオ /, MAKIMOTO, Hiroshi, ASAMI, Masao, GREW, Edward S.
Language:English
Published: National Institute of Polar Research 1989
Subjects:
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
_version_ 1829310824475262976
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