Deformation of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica

P(論文) The deformation history of ultrahigh-temperature metamorphic rocks from Tonagh Island, Napier Complex, East Antarctica is divided into nine stages, namely D_1 to D_9. The D_1 structure would have been formed under non- or weakly-deformational condition during thermal peak of prograde metamorph...

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Main Authors: Toyoshima, Tsuyoshi, Osanai, Yasuhito, Owada, Masaaki, Tsunogae, Toshiaki, Hokada, Tomokazu, Crowe, Warwick A.
Language:English
Published: National Institute of Polar Research 1999
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3041/files/KJ00000044158.pdf
https://doi.org/10.15094/00003041
https://nipr.repo.nii.ac.jp/records/3041
_version_ 1829298016622739456
author Toyoshima, Tsuyoshi
Osanai, Yasuhito
Owada, Masaaki
Tsunogae, Toshiaki
Hokada, Tomokazu
Crowe, Warwick A.
author_facet Toyoshima, Tsuyoshi
Osanai, Yasuhito
Owada, Masaaki
Tsunogae, Toshiaki
Hokada, Tomokazu
Crowe, Warwick A.
author_sort Toyoshima, Tsuyoshi
collection National Institute of Polar Research Repository, Japan
description P(論文) The deformation history of ultrahigh-temperature metamorphic rocks from Tonagh Island, Napier Complex, East Antarctica is divided into nine stages, namely D_1 to D_9. The D_1 structure would have been formed under non- or weakly-deformational condition during thermal peak of prograde metamorphism. The D_2-D_6 structures would have been produced under retrograde granulite facies conditions. Subsequently D_7-D_9 brittle faulting modified the structures in part. The D_1 to D_8 deformation corresponds to first to third tectonometamorphic episodes, previously reported, of the whole Napier Complex before the intrusion of the Amundsen dyke. The structural geology of the Island is mainly characterized by NE-SW trending D_2 foliation (S_2) with WNW plunging mineral lineation, WNW-ESE to E-W trending D_5 folds and NE-SW to E-W trending D_6 mylonite zones. S_2 is the main foliation of this area, but was highly folded and faulted during the D_5-D_6 stages. The S_2 and S_2-parallel D_3 shear zones are the products of layer-parallel shearing due to a top-to-the-SE (dextral-reverse) displacement. The D_3 and D_6 fault rocks show that seismic faulting and plastic deformation alternated both during the D_3 stage and during the D_6 stage under retrograde granulite facies conditions. Multiphase faulting in different shear senses occurred during the D_6 stage. departmental bulletin paper
genre Antarc*
Antarctica
East Antarctica
Polar geoscience
Tonagh Island
genre_facet Antarc*
Antarctica
East Antarctica
Polar geoscience
Tonagh Island
geographic East Antarctica
Napier
Tonagh Island
geographic_facet East Antarctica
Napier
Tonagh Island
id ftnipr:oai:nipr.repo.nii.ac.jp:00003041
institution Open Polar
language English
long_lat ENVELOPE(-58.440,-58.440,-62.167,-62.167)
ENVELOPE(50.333,50.333,-67.117,-67.117)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003041
op_relation Polar geoscience
12
29
48
AA1130866X
https://nipr.repo.nii.ac.jp/record/3041/files/KJ00000044158.pdf
https://doi.org/10.15094/00003041
https://nipr.repo.nii.ac.jp/records/3041
publishDate 1999
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003041 2025-04-13T14:08:48+00:00 Deformation of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica Toyoshima, Tsuyoshi Osanai, Yasuhito Owada, Masaaki Tsunogae, Toshiaki Hokada, Tomokazu Crowe, Warwick A. 1999-10 application/pdf https://nipr.repo.nii.ac.jp/record/3041/files/KJ00000044158.pdf https://doi.org/10.15094/00003041 https://nipr.repo.nii.ac.jp/records/3041 eng eng National Institute of Polar Research Polar geoscience 12 29 48 AA1130866X https://nipr.repo.nii.ac.jp/record/3041/files/KJ00000044158.pdf https://doi.org/10.15094/00003041 https://nipr.repo.nii.ac.jp/records/3041 Napier Complex ultrahigh-temperature deformation mylonite foliated pseudotachylyte deformation history 1999 ftnipr https://doi.org/10.15094/00003041 2025-03-19T10:19:56Z P(論文) The deformation history of ultrahigh-temperature metamorphic rocks from Tonagh Island, Napier Complex, East Antarctica is divided into nine stages, namely D_1 to D_9. The D_1 structure would have been formed under non- or weakly-deformational condition during thermal peak of prograde metamorphism. The D_2-D_6 structures would have been produced under retrograde granulite facies conditions. Subsequently D_7-D_9 brittle faulting modified the structures in part. The D_1 to D_8 deformation corresponds to first to third tectonometamorphic episodes, previously reported, of the whole Napier Complex before the intrusion of the Amundsen dyke. The structural geology of the Island is mainly characterized by NE-SW trending D_2 foliation (S_2) with WNW plunging mineral lineation, WNW-ESE to E-W trending D_5 folds and NE-SW to E-W trending D_6 mylonite zones. S_2 is the main foliation of this area, but was highly folded and faulted during the D_5-D_6 stages. The S_2 and S_2-parallel D_3 shear zones are the products of layer-parallel shearing due to a top-to-the-SE (dextral-reverse) displacement. The D_3 and D_6 fault rocks show that seismic faulting and plastic deformation alternated both during the D_3 stage and during the D_6 stage under retrograde granulite facies conditions. Multiphase faulting in different shear senses occurred during the D_6 stage. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica Polar geoscience Tonagh Island National Institute of Polar Research Repository, Japan East Antarctica Napier ENVELOPE(-58.440,-58.440,-62.167,-62.167) Tonagh Island ENVELOPE(50.333,50.333,-67.117,-67.117)
spellingShingle Napier Complex
ultrahigh-temperature deformation
mylonite
foliated pseudotachylyte
deformation history
Toyoshima, Tsuyoshi
Osanai, Yasuhito
Owada, Masaaki
Tsunogae, Toshiaki
Hokada, Tomokazu
Crowe, Warwick A.
Deformation of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica
title Deformation of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica
title_full Deformation of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica
title_fullStr Deformation of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica
title_full_unstemmed Deformation of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica
title_short Deformation of ultrahigh-temperature metamorphic rocks from Tonagh Island in the Napier Complex, East Antarctica
title_sort deformation of ultrahigh-temperature metamorphic rocks from tonagh island in the napier complex, east antarctica
topic Napier Complex
ultrahigh-temperature deformation
mylonite
foliated pseudotachylyte
deformation history
topic_facet Napier Complex
ultrahigh-temperature deformation
mylonite
foliated pseudotachylyte
deformation history
url https://nipr.repo.nii.ac.jp/record/3041/files/KJ00000044158.pdf
https://doi.org/10.15094/00003041
https://nipr.repo.nii.ac.jp/records/3041