Geology of the Sandercock Nunataks in Enderby Land, East Antarctica (Reports of the Japanese Antarctic Research Expedition)
The Sandercock. Nunataks (68°33'S, 52°07'E) are composed of several small nunataks which are tentatively named A, B, C and D. Nunatak "A" consists mainly of hornblende-biotite gneiss and Nunatak "B" of hypersthene-garnet gneiss and garnet gneiss. Nunatak "C" i...
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Format: | Article |
Language: | English |
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National Institute of Polar Research
1972-11-01
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Series: | Antarctic Record |
Online Access: | https://doi.org/10.15094/00007688 |
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author | Kazuyuki SHIRAISHI Okitsugu WATANABE Koshiro KIZAKI |
author_facet | Kazuyuki SHIRAISHI Okitsugu WATANABE Koshiro KIZAKI |
author_sort | Kazuyuki SHIRAISHI |
collection | DOAJ |
description | The Sandercock. Nunataks (68°33'S, 52°07'E) are composed of several small nunataks which are tentatively named A, B, C and D. Nunatak "A" consists mainly of hornblende-biotite gneiss and Nunatak "B" of hypersthene-garnet gneiss and garnet gneiss. Nunatak "C" is composed of hypersthene-hornblende gneiss. They are associated with aplites, pegmatites and metabasites. The petrographic observations under the microscope reveal that the unstable hypersthene signifies the transition of the granulite facies conditions to the amphibolite facies conditions. The transition is not unusual throughout the East Antarctic platform, particularly in the Lutzow-Holm Bukt area and Queen Maud Land. |
first_indexed | 2024-12-20T09:59:59Z |
format | Article |
id | doaj.art-6c8db63505f14651b9f0831f7b441b18 |
institution | Directory Open Access Journal |
issn | 0085-7289 2432-079X |
language | English |
last_indexed | 2024-12-20T09:59:59Z |
publishDate | 1972-11-01 |
publisher | National Institute of Polar Research |
record_format | Article |
series | Antarctic Record |
spelling | doaj.art-6c8db63505f14651b9f0831f7b441b182022-12-21T19:44:21ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X1972-11-0145667510.15094/00007688Geology of the Sandercock Nunataks in Enderby Land, East Antarctica (Reports of the Japanese Antarctic Research Expedition)Kazuyuki SHIRAISHI0Okitsugu WATANABE1Koshiro KIZAKI2Faculty of Science, Hokkaido UniversityWater Research Laboratory, Nagoya UniversityCollege of General Education, Ryukyu UniversityThe Sandercock. Nunataks (68°33'S, 52°07'E) are composed of several small nunataks which are tentatively named A, B, C and D. Nunatak "A" consists mainly of hornblende-biotite gneiss and Nunatak "B" of hypersthene-garnet gneiss and garnet gneiss. Nunatak "C" is composed of hypersthene-hornblende gneiss. They are associated with aplites, pegmatites and metabasites. The petrographic observations under the microscope reveal that the unstable hypersthene signifies the transition of the granulite facies conditions to the amphibolite facies conditions. The transition is not unusual throughout the East Antarctic platform, particularly in the Lutzow-Holm Bukt area and Queen Maud Land.https://doi.org/10.15094/00007688 |
spellingShingle | Kazuyuki SHIRAISHI Okitsugu WATANABE Koshiro KIZAKI Geology of the Sandercock Nunataks in Enderby Land, East Antarctica (Reports of the Japanese Antarctic Research Expedition) Antarctic Record |
title | Geology of the Sandercock Nunataks in Enderby Land, East Antarctica (Reports of the Japanese Antarctic Research Expedition) |
title_full | Geology of the Sandercock Nunataks in Enderby Land, East Antarctica (Reports of the Japanese Antarctic Research Expedition) |
title_fullStr | Geology of the Sandercock Nunataks in Enderby Land, East Antarctica (Reports of the Japanese Antarctic Research Expedition) |
title_full_unstemmed | Geology of the Sandercock Nunataks in Enderby Land, East Antarctica (Reports of the Japanese Antarctic Research Expedition) |
title_short | Geology of the Sandercock Nunataks in Enderby Land, East Antarctica (Reports of the Japanese Antarctic Research Expedition) |
title_sort | geology of the sandercock nunataks in enderby land east antarctica reports of the japanese antarctic research expedition |
url | https://doi.org/10.15094/00007688 |
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