Geology of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica
The summer party of the 39th Japanese Antarctic Research Expedition (1997-1998) carried out geological field work on Tonagh Island, located at the southern-end of Amundsen Bay, northern Enderby Land, which belongs to the central Napier Complex and shows part of the highest-grade metamorphic region i...
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ftnipr:oai:nipr.repo.nii.ac.jp:00003040 2023-05-15T13:22:48+02:00 Geology of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica Yasuhito Osanai Tsuyoshi Toyoshima Masaaki Owada Toshiaki Tsunogae Tomokazu Hokada Warwick A. Crowe 1999-10 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3040 http://id.nii.ac.jp/1291/00003040/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3040&item_no=1&attribute_id=18&file_no=1 en eng Department of Earth Sciences, Okayama University/Graduate School of Science and Technology, Niigata University/Department of Earth Sciences, Yamaguchi University/Department of Earth Sciences, Shimane University/Department of Polar Science, School of Mathematical and Physical Sciences, The Graduate University for Advanced Studies/Department of Geology and Geophysics, University of Western Australia National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3040 http://id.nii.ac.jp/1291/00003040/ AA1130866X Polar geoscience, 12, 1-28(1999-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3040&item_no=1&attribute_id=18&file_no=1 Archaean Napier Complex Tonagh Island regional geology UHT metamorphic rocks Departmental Bulletin Paper P(論文) 1999 ftnipr 2022-11-26T19:42:23Z The summer party of the 39th Japanese Antarctic Research Expedition (1997-1998) carried out geological field work on Tonagh Island, located at the southern-end of Amundsen Bay, northern Enderby Land, which belongs to the central Napier Complex and shows part of the highest-grade metamorphic region in the Napier Complex. The island is underlain by various kinds of ultrahigh-temperature (UHT) metamorphic rocks and subordinate amounts of two types of unmetamorphosed intrusive rocks (alkali-dolerite and granitic pegmatite). UHT-metamorphic rocks are subdivided into five lithologic units (Units I to V) owing to their lithologies and geological structures from north to south, bounded by thrust-shear zones, accompanied with remarkable anhydrous mylonite and later pseudotachylite-cataclasite. The distinctive metamorphosed mafic dikes with tholeiitic composition are also found along the shear zone, characteristically at the boundary between Units II and III. The unmetamorphosed alkali-dolerite dikes, which are designated Amundsen dikes, cut across not only the sequence of metamorphic rocks but also the unit boundary shear zone and metamorphosed mafic dike. A geological perspective of the metamorphic rocks from Tonagh Island is generally classified into eight types on the regional map scale such as 1) orthopyroxene-bearing quartzofeldspathic gneiss, 2) garnet-bearing quartzofeldspathic gneiss, 3) two pyroxene-bearing mafic granulite, 4) garnet-orthopyroxene gneiss and granulite, 5) magnetite-quartz gneiss, 6) metamorphosed ultramafic rocks, 7) layered gneiss 1 (composed mainly of mafic gneiss and orthopyroxene-bearing quartzofeldspathic gneiss), 8) layered gneiss 2 (composed mainly of mafic gneiss and garnet-bearing quartzofeldspathic gneiss) with subordinate meta-impure quartzite, aluminous granulite, and calc-silicate granulite. The orthopyroxene-bearing quartzofeldspathic charnockitic gneiss and garnet-bearing quartzofeldspathic gneiss are the main constituents of Tonagh Island. Unit I has a peculiarity of predominance ... Report Amundsen Bay Antarc* Antarctic Antarctica East Antarctica Enderby Land Polar geoscience Tonagh Island National Institute of Polar Research Repository, Japan Antarctic East Antarctica Napier ENVELOPE(-58.440,-58.440,-62.167,-62.167) Amundsen Bay ENVELOPE(50.000,50.000,-66.917,-66.917) Tonagh Island ENVELOPE(50.333,50.333,-67.117,-67.117) |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
topic |
Archaean Napier Complex Tonagh Island regional geology UHT metamorphic rocks |
spellingShingle |
Archaean Napier Complex Tonagh Island regional geology UHT metamorphic rocks Yasuhito Osanai Tsuyoshi Toyoshima Masaaki Owada Toshiaki Tsunogae Tomokazu Hokada Warwick A. Crowe Geology of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica |
topic_facet |
Archaean Napier Complex Tonagh Island regional geology UHT metamorphic rocks |
description |
The summer party of the 39th Japanese Antarctic Research Expedition (1997-1998) carried out geological field work on Tonagh Island, located at the southern-end of Amundsen Bay, northern Enderby Land, which belongs to the central Napier Complex and shows part of the highest-grade metamorphic region in the Napier Complex. The island is underlain by various kinds of ultrahigh-temperature (UHT) metamorphic rocks and subordinate amounts of two types of unmetamorphosed intrusive rocks (alkali-dolerite and granitic pegmatite). UHT-metamorphic rocks are subdivided into five lithologic units (Units I to V) owing to their lithologies and geological structures from north to south, bounded by thrust-shear zones, accompanied with remarkable anhydrous mylonite and later pseudotachylite-cataclasite. The distinctive metamorphosed mafic dikes with tholeiitic composition are also found along the shear zone, characteristically at the boundary between Units II and III. The unmetamorphosed alkali-dolerite dikes, which are designated Amundsen dikes, cut across not only the sequence of metamorphic rocks but also the unit boundary shear zone and metamorphosed mafic dike. A geological perspective of the metamorphic rocks from Tonagh Island is generally classified into eight types on the regional map scale such as 1) orthopyroxene-bearing quartzofeldspathic gneiss, 2) garnet-bearing quartzofeldspathic gneiss, 3) two pyroxene-bearing mafic granulite, 4) garnet-orthopyroxene gneiss and granulite, 5) magnetite-quartz gneiss, 6) metamorphosed ultramafic rocks, 7) layered gneiss 1 (composed mainly of mafic gneiss and orthopyroxene-bearing quartzofeldspathic gneiss), 8) layered gneiss 2 (composed mainly of mafic gneiss and garnet-bearing quartzofeldspathic gneiss) with subordinate meta-impure quartzite, aluminous granulite, and calc-silicate granulite. The orthopyroxene-bearing quartzofeldspathic charnockitic gneiss and garnet-bearing quartzofeldspathic gneiss are the main constituents of Tonagh Island. Unit I has a peculiarity of predominance ... |
format |
Report |
author |
Yasuhito Osanai Tsuyoshi Toyoshima Masaaki Owada Toshiaki Tsunogae Tomokazu Hokada Warwick A. Crowe |
author_facet |
Yasuhito Osanai Tsuyoshi Toyoshima Masaaki Owada Toshiaki Tsunogae Tomokazu Hokada Warwick A. Crowe |
author_sort |
Yasuhito Osanai |
title |
Geology of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica |
title_short |
Geology of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica |
title_full |
Geology of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica |
title_fullStr |
Geology of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica |
title_full_unstemmed |
Geology of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica |
title_sort |
geology of ultrahigh-temperature metamorphic rocks from tonagh island in the napier complex, east antarctica |
publisher |
Department of Earth Sciences, Okayama University/Graduate School of Science and Technology, Niigata University/Department of Earth Sciences, Yamaguchi University/Department of Earth Sciences, Shimane University/Department of Polar Science, School of Mathematical and Physical Sciences, The Graduate University for Advanced Studies/Department of Geology and Geophysics, University of Western Australia |
publishDate |
1999 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3040 http://id.nii.ac.jp/1291/00003040/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3040&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(-58.440,-58.440,-62.167,-62.167) ENVELOPE(50.000,50.000,-66.917,-66.917) ENVELOPE(50.333,50.333,-67.117,-67.117) |
geographic |
Antarctic East Antarctica Napier Amundsen Bay Tonagh Island |
geographic_facet |
Antarctic East Antarctica Napier Amundsen Bay Tonagh Island |
genre |
Amundsen Bay Antarc* Antarctic Antarctica East Antarctica Enderby Land Polar geoscience Tonagh Island |
genre_facet |
Amundsen Bay Antarc* Antarctic Antarctica East Antarctica Enderby Land Polar geoscience Tonagh Island |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3040 http://id.nii.ac.jp/1291/00003040/ AA1130866X Polar geoscience, 12, 1-28(1999-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3040&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766367028562624512 |