High-grade metamorphic rocks from Christmas Point in the Napier Complex, East Antarctica
The Christmas Point area is dominated by well-layered gneisses, of which garnet-orthopyroxene gneiss and garnet felsic gneiss are the most abundant types. Orthopyroxene-bearing quartz-rich granulite, layering of which is indistinct to massive, is present as layers within the garnet felsic gneiss. Ga...
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ftnipr:oai:nipr.repo.nii.ac.jp:00003085 2023-05-15T13:49:00+02:00 High-grade metamorphic rocks from Christmas Point in the Napier Complex, East Antarctica Yasutaka Yoshimura Tomoharu Miyamoto Edward S. Grew Christopher J. Carson Daniel J. Dunkley Yoichi Motoyoshi 2001-10 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3085 http://id.nii.ac.jp/1291/00003085/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3085&item_no=1&attribute_id=18&file_no=1 en eng Department of Natural Environmental Science, Kochi University/Department of Earth and Planetary Science, Kyushu University/Department of Geological Science, University of Maine/Department of Geology and Geophysics, Kline Geology Laboratory, Yale University/School of Geosciences, Edgeworth David Building, University of Sydney/National Institute of Polar Research National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3085 http://id.nii.ac.jp/1291/00003085/ AA1130866X Polar geoscience, 14, 53-74(2001-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3085&item_no=1&attribute_id=18&file_no=1 UHT metamorphic rocks UHT metamorphism Christmas Point Napier Complex East Antarctica Departmental Bulletin Paper P(論文) 2001 ftnipr 2022-11-26T19:42:23Z The Christmas Point area is dominated by well-layered gneisses, of which garnet-orthopyroxene gneiss and garnet felsic gneiss are the most abundant types. Orthopyroxene-bearing quartz-rich granulite, layering of which is indistinct to massive, is present as layers within the garnet felsic gneiss. Garnet-amphibole gneiss is present as layers in both the garnet-orthopyroxene gneiss and the garnet felsic gneiss. Orthopyroxene-bearing quartz-rich granulites contain coexisting orthopyroxene, sillimanite and quartz. The occurrence of sapphirine as inclusions in sillimanite implies that metamorphic conditions changed from the stability field of sapphirine+quartz to that of orthopyroxene+sillimanite+quartz. P-T conditions estimated using garnet-orthopyroxene geothermobarometry range from 920 to 1040℃ and 8.8 to 11.5 kbar. Garnet exsolution lamellae present in orthopyroxene from the garnet-orthopyroxene gneiss suggest that a precursor aluminous orthopyroxene was present during the ultrahigh-temperature stage. For the retrograde event, although chemical zoning of major element composition of garnet developed during cooling and reflects high-temperature diffusion, compositional zoning of more slowly diffusing elements, such as Ca, show a complicated pattern caused by partial resorbtion and overgrowth. Garnet rims in all rock types are intergrown with quartz and have relatively high grossular composition. Plagioclase in the garnet-orthopyroxene gneiss and garnet felsic gneiss show reverse zoning. Garnet-amphibole gneiss contains two amphiboles (gedrite and cummingtonite) with different fluorine contents; gedrite occurs as finely crystalline overgrowths surrounding cummingtonite, implying that the retrograde process after peak (ultrahigh-temperature) metamorphism was not simple cooling. Report Antarc* Antarctica East Antarctica Polar geoscience National Institute of Polar Research Repository, Japan East Antarctica Napier ENVELOPE(-58.440,-58.440,-62.167,-62.167) Christmas Point ENVELOPE(48.967,48.967,-67.383,-67.383) |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
topic |
UHT metamorphic rocks UHT metamorphism Christmas Point Napier Complex East Antarctica |
spellingShingle |
UHT metamorphic rocks UHT metamorphism Christmas Point Napier Complex East Antarctica Yasutaka Yoshimura Tomoharu Miyamoto Edward S. Grew Christopher J. Carson Daniel J. Dunkley Yoichi Motoyoshi High-grade metamorphic rocks from Christmas Point in the Napier Complex, East Antarctica |
topic_facet |
UHT metamorphic rocks UHT metamorphism Christmas Point Napier Complex East Antarctica |
description |
The Christmas Point area is dominated by well-layered gneisses, of which garnet-orthopyroxene gneiss and garnet felsic gneiss are the most abundant types. Orthopyroxene-bearing quartz-rich granulite, layering of which is indistinct to massive, is present as layers within the garnet felsic gneiss. Garnet-amphibole gneiss is present as layers in both the garnet-orthopyroxene gneiss and the garnet felsic gneiss. Orthopyroxene-bearing quartz-rich granulites contain coexisting orthopyroxene, sillimanite and quartz. The occurrence of sapphirine as inclusions in sillimanite implies that metamorphic conditions changed from the stability field of sapphirine+quartz to that of orthopyroxene+sillimanite+quartz. P-T conditions estimated using garnet-orthopyroxene geothermobarometry range from 920 to 1040℃ and 8.8 to 11.5 kbar. Garnet exsolution lamellae present in orthopyroxene from the garnet-orthopyroxene gneiss suggest that a precursor aluminous orthopyroxene was present during the ultrahigh-temperature stage. For the retrograde event, although chemical zoning of major element composition of garnet developed during cooling and reflects high-temperature diffusion, compositional zoning of more slowly diffusing elements, such as Ca, show a complicated pattern caused by partial resorbtion and overgrowth. Garnet rims in all rock types are intergrown with quartz and have relatively high grossular composition. Plagioclase in the garnet-orthopyroxene gneiss and garnet felsic gneiss show reverse zoning. Garnet-amphibole gneiss contains two amphiboles (gedrite and cummingtonite) with different fluorine contents; gedrite occurs as finely crystalline overgrowths surrounding cummingtonite, implying that the retrograde process after peak (ultrahigh-temperature) metamorphism was not simple cooling. |
format |
Report |
author |
Yasutaka Yoshimura Tomoharu Miyamoto Edward S. Grew Christopher J. Carson Daniel J. Dunkley Yoichi Motoyoshi |
author_facet |
Yasutaka Yoshimura Tomoharu Miyamoto Edward S. Grew Christopher J. Carson Daniel J. Dunkley Yoichi Motoyoshi |
author_sort |
Yasutaka Yoshimura |
title |
High-grade metamorphic rocks from Christmas Point in the Napier Complex, East Antarctica |
title_short |
High-grade metamorphic rocks from Christmas Point in the Napier Complex, East Antarctica |
title_full |
High-grade metamorphic rocks from Christmas Point in the Napier Complex, East Antarctica |
title_fullStr |
High-grade metamorphic rocks from Christmas Point in the Napier Complex, East Antarctica |
title_full_unstemmed |
High-grade metamorphic rocks from Christmas Point in the Napier Complex, East Antarctica |
title_sort |
high-grade metamorphic rocks from christmas point in the napier complex, east antarctica |
publisher |
Department of Natural Environmental Science, Kochi University/Department of Earth and Planetary Science, Kyushu University/Department of Geological Science, University of Maine/Department of Geology and Geophysics, Kline Geology Laboratory, Yale University/School of Geosciences, Edgeworth David Building, University of Sydney/National Institute of Polar Research |
publishDate |
2001 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3085 http://id.nii.ac.jp/1291/00003085/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3085&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(-58.440,-58.440,-62.167,-62.167) ENVELOPE(48.967,48.967,-67.383,-67.383) |
geographic |
East Antarctica Napier Christmas Point |
geographic_facet |
East Antarctica Napier Christmas Point |
genre |
Antarc* Antarctica East Antarctica Polar geoscience |
genre_facet |
Antarc* Antarctica East Antarctica Polar geoscience |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3085 http://id.nii.ac.jp/1291/00003085/ AA1130866X Polar geoscience, 14, 53-74(2001-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3085&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250343245545472 |