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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Main Authors: Kazuyuki SHIRAISHI, Okitsugu WATANABE, Koshiro KIZAKI
Format: Article
Language:English
Published: National Institute of Polar Research 1972-11-01
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.
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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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