PEGMATITE FROM NESOYA ISLAND, LUTZOW-HOLM BAY, EAST ANTARCTICA : WITH SPECIAL REFERENCE TO GARNET-QUARTZ SYMPLEKTITE
Graphic intergrowth of garnet and quartz occurs in Nesoya Island on the north of Syowa Station, East Antarctica. The intergrowth occupies small domains in microcline pegmatite dykes, which yield metamict cerianite and obliquely cut the basement gneisses and hornblende pegmatite. In the domains, redd...
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ftnipr:oai:nipr.repo.nii.ac.jp:00002604 2023-05-15T13:48:59+02:00 PEGMATITE FROM NESOYA ISLAND, LUTZOW-HOLM BAY, EAST ANTARCTICA : WITH SPECIAL REFERENCE TO GARNET-QUARTZ SYMPLEKTITE スズキ モリヒサ マツモト ユキオ Morihisa SUZUKI Yukio MATSUMOTO 1989-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2604 http://id.nii.ac.jp/1291/00002604/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2604&item_no=1&attribute_id=18&file_no=1 en eng ABSTRACT Department of Geology, Faculty of School Education, Hiroshima University Department of Mineralogical Sciences and Geology, Faculty of Science, Yamaguchi University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2604 http://id.nii.ac.jp/1291/00002604/ AA1072335X Proceedings of the NIPR Symposium on Antarctic Geosciences, 3, 151(1989-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2604&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1989 ftnipr 2022-11-19T19:41:20Z Graphic intergrowth of garnet and quartz occurs in Nesoya Island on the north of Syowa Station, East Antarctica. The intergrowth occupies small domains in microcline pegmatite dykes, which yield metamict cerianite and obliquely cut the basement gneisses and hornblende pegmatite. In the domains, reddish garnet and smoky quartz are in an interfingering relationship with the width of several millimeters. Fe-Ti oxides, K-feldspar and biotite are absent in the domains. Garnet shows a weakly-zoned structure with a rather Ca-rich core, namely, the rim attached to quartz and plagioclase has the composition of Gros_<14.1>Alm_<72.4>Pyr_<6.0>Spes_<7.2> and the core Gros_<16.1>Alm_<71.2>Pyr_<5.5>Spes_<7.2>. The low pyrope content is in contrast to the higher value in garnet from gneisses around Syowa Station, ranging from 18 to 46. Plagioclase occurs as an irregularly-shaped crystal in a narrow area along the rim of garnet. It is also zoned with a rather Ca-poor core (An=22.3) fringed by the rim (An=23.6-23.8). Or content is lower than 2.8 in both core and rim. Judged from the texture, chemical composition and mineral species associated, it is inferred that the intergrowth has not formed through the interaction of quartzo-feldspathic magma with garnet in surrounding gneisses but directly crystallized from the magma. It seems possible that the crystallization has proceeded under rather low fo_2 condition, because the pegmatite contains no Fe-Ti oxides such as magnetite. Report Antarc* Antarctica East Antarctica National Institute of Polar Research Repository, Japan East Antarctica Syowa Station Nesoya ENVELOPE(39.567,39.567,-69.000,-69.000) |
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Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
Graphic intergrowth of garnet and quartz occurs in Nesoya Island on the north of Syowa Station, East Antarctica. The intergrowth occupies small domains in microcline pegmatite dykes, which yield metamict cerianite and obliquely cut the basement gneisses and hornblende pegmatite. In the domains, reddish garnet and smoky quartz are in an interfingering relationship with the width of several millimeters. Fe-Ti oxides, K-feldspar and biotite are absent in the domains. Garnet shows a weakly-zoned structure with a rather Ca-rich core, namely, the rim attached to quartz and plagioclase has the composition of Gros_<14.1>Alm_<72.4>Pyr_<6.0>Spes_<7.2> and the core Gros_<16.1>Alm_<71.2>Pyr_<5.5>Spes_<7.2>. The low pyrope content is in contrast to the higher value in garnet from gneisses around Syowa Station, ranging from 18 to 46. Plagioclase occurs as an irregularly-shaped crystal in a narrow area along the rim of garnet. It is also zoned with a rather Ca-poor core (An=22.3) fringed by the rim (An=23.6-23.8). Or content is lower than 2.8 in both core and rim. Judged from the texture, chemical composition and mineral species associated, it is inferred that the intergrowth has not formed through the interaction of quartzo-feldspathic magma with garnet in surrounding gneisses but directly crystallized from the magma. It seems possible that the crystallization has proceeded under rather low fo_2 condition, because the pegmatite contains no Fe-Ti oxides such as magnetite. |
format |
Report |
author |
スズキ モリヒサ マツモト ユキオ Morihisa SUZUKI Yukio MATSUMOTO |
spellingShingle |
スズキ モリヒサ マツモト ユキオ Morihisa SUZUKI Yukio MATSUMOTO PEGMATITE FROM NESOYA ISLAND, LUTZOW-HOLM BAY, EAST ANTARCTICA : WITH SPECIAL REFERENCE TO GARNET-QUARTZ SYMPLEKTITE |
author_facet |
スズキ モリヒサ マツモト ユキオ Morihisa SUZUKI Yukio MATSUMOTO |
author_sort |
スズキ モリヒサ |
title |
PEGMATITE FROM NESOYA ISLAND, LUTZOW-HOLM BAY, EAST ANTARCTICA : WITH SPECIAL REFERENCE TO GARNET-QUARTZ SYMPLEKTITE |
title_short |
PEGMATITE FROM NESOYA ISLAND, LUTZOW-HOLM BAY, EAST ANTARCTICA : WITH SPECIAL REFERENCE TO GARNET-QUARTZ SYMPLEKTITE |
title_full |
PEGMATITE FROM NESOYA ISLAND, LUTZOW-HOLM BAY, EAST ANTARCTICA : WITH SPECIAL REFERENCE TO GARNET-QUARTZ SYMPLEKTITE |
title_fullStr |
PEGMATITE FROM NESOYA ISLAND, LUTZOW-HOLM BAY, EAST ANTARCTICA : WITH SPECIAL REFERENCE TO GARNET-QUARTZ SYMPLEKTITE |
title_full_unstemmed |
PEGMATITE FROM NESOYA ISLAND, LUTZOW-HOLM BAY, EAST ANTARCTICA : WITH SPECIAL REFERENCE TO GARNET-QUARTZ SYMPLEKTITE |
title_sort |
pegmatite from nesoya island, lutzow-holm bay, east antarctica : with special reference to garnet-quartz symplektite |
publisher |
ABSTRACT |
publishDate |
1989 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2604 http://id.nii.ac.jp/1291/00002604/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2604&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(39.567,39.567,-69.000,-69.000) |
geographic |
East Antarctica Syowa Station Nesoya |
geographic_facet |
East Antarctica Syowa Station Nesoya |
genre |
Antarc* Antarctica East Antarctica |
genre_facet |
Antarc* Antarctica East Antarctica |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2604 http://id.nii.ac.jp/1291/00002604/ AA1072335X Proceedings of the NIPR Symposium on Antarctic Geosciences, 3, 151(1989-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2604&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250286254391296 |