Experimental constraints on partial melting under UHT and dry conditions of quartzo-feldspathic rock in the Napier Complex, East Antarctica

P(論文) We carried out high pressure melting experiments on a mixture of mineral separates of quartz, plagioclase (antiperthite) and a rare amount of orthopyroxene at 1000-1150℃ and 1.0 Gpa under dry conditions. The starting material was obtained from an ultrahigh-temperature (UHT) garnet-orthopyroxen...

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Main Authors: Hokada, Tomokazu, Arima, Makoto
Language:English
Published: National Institute of Polar Research 2001
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3084/files/KJ00000044202.pdf
https://doi.org/10.15094/00003084
https://nipr.repo.nii.ac.jp/records/3084
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author Hokada, Tomokazu
Arima, Makoto
author_facet Hokada, Tomokazu
Arima, Makoto
author_sort Hokada, Tomokazu
collection National Institute of Polar Research Repository, Japan
description P(論文) We carried out high pressure melting experiments on a mixture of mineral separates of quartz, plagioclase (antiperthite) and a rare amount of orthopyroxene at 1000-1150℃ and 1.0 Gpa under dry conditions. The starting material was obtained from an ultrahigh-temperature (UHT) garnet-orthopyroxene-bearing quartzo-feldspathic gneiss in the Mt. Riiser-Larsen of the Napier Complex, East Antarctica. This UHT gneiss is considered to be equilibrated at metamorphic conditions >1070℃. The mineral assemblages in the run products at 1000℃ and 1100℃ are the same as those of the starting material. K_2O content in K-feldspar lamellae of antiperthite decreases with temperature. Granitic glass (<10 vol%) was detected along boundaries between lamella-free plagioclase and quartz grains in the run at 1150℃. The experimental results indicate that the homogenization temperature of this antiperthite lies <1150℃ at 1.0 Gpa. It is consistent with the estimated temperature from feldspar geothermometry. Major element composition of the glass at 1150℃ shows the molecular Al_2O_3/(Na_2O+K_2O+CaO) ratio (A.S.I.: aluminum saturation index) = 1.08 and high Na_2O+K_2O contents (8.1 wt%) relative to low CaO (1.3 wt%), which is comparable to the chemical features of A-type granite or leucogranite. This may imply that some genetic links might exist between UHT metamorphism and A-type granite magmatism in the Napier Complex. departmental bulletin paper
genre Antarc*
Antarctica
East Antarctica
Polar geoscience
genre_facet Antarc*
Antarctica
East Antarctica
Polar geoscience
geographic East Antarctica
Riiser-Larsen
Napier
geographic_facet East Antarctica
Riiser-Larsen
Napier
id ftnipr:oai:nipr.repo.nii.ac.jp:00003084
institution Open Polar
language English
long_lat ENVELOPE(50.667,50.667,-66.783,-66.783)
ENVELOPE(-58.440,-58.440,-62.167,-62.167)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003084
op_relation Polar geoscience
14
39
52
AA1130866X
https://nipr.repo.nii.ac.jp/record/3084/files/KJ00000044202.pdf
https://doi.org/10.15094/00003084
https://nipr.repo.nii.ac.jp/records/3084
publishDate 2001
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003084 2025-04-13T14:09:28+00:00 Experimental constraints on partial melting under UHT and dry conditions of quartzo-feldspathic rock in the Napier Complex, East Antarctica Hokada, Tomokazu Arima, Makoto 2001-10 application/pdf https://nipr.repo.nii.ac.jp/record/3084/files/KJ00000044202.pdf https://doi.org/10.15094/00003084 https://nipr.repo.nii.ac.jp/records/3084 eng eng National Institute of Polar Research Polar geoscience 14 39 52 AA1130866X https://nipr.repo.nii.ac.jp/record/3084/files/KJ00000044202.pdf https://doi.org/10.15094/00003084 https://nipr.repo.nii.ac.jp/records/3084 dry condition feldspar melting experiment Napier Complex ultrahigh-temperature (UHT) metamorphism 2001 ftnipr https://doi.org/10.15094/00003084 2025-03-19T10:19:57Z P(論文) We carried out high pressure melting experiments on a mixture of mineral separates of quartz, plagioclase (antiperthite) and a rare amount of orthopyroxene at 1000-1150℃ and 1.0 Gpa under dry conditions. The starting material was obtained from an ultrahigh-temperature (UHT) garnet-orthopyroxene-bearing quartzo-feldspathic gneiss in the Mt. Riiser-Larsen of the Napier Complex, East Antarctica. This UHT gneiss is considered to be equilibrated at metamorphic conditions >1070℃. The mineral assemblages in the run products at 1000℃ and 1100℃ are the same as those of the starting material. K_2O content in K-feldspar lamellae of antiperthite decreases with temperature. Granitic glass (<10 vol%) was detected along boundaries between lamella-free plagioclase and quartz grains in the run at 1150℃. The experimental results indicate that the homogenization temperature of this antiperthite lies <1150℃ at 1.0 Gpa. It is consistent with the estimated temperature from feldspar geothermometry. Major element composition of the glass at 1150℃ shows the molecular Al_2O_3/(Na_2O+K_2O+CaO) ratio (A.S.I.: aluminum saturation index) = 1.08 and high Na_2O+K_2O contents (8.1 wt%) relative to low CaO (1.3 wt%), which is comparable to the chemical features of A-type granite or leucogranite. This may imply that some genetic links might exist between UHT metamorphism and A-type granite magmatism in the Napier Complex. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica Polar geoscience National Institute of Polar Research Repository, Japan East Antarctica Riiser-Larsen ENVELOPE(50.667,50.667,-66.783,-66.783) Napier ENVELOPE(-58.440,-58.440,-62.167,-62.167)
spellingShingle dry condition
feldspar
melting experiment
Napier Complex
ultrahigh-temperature (UHT) metamorphism
Hokada, Tomokazu
Arima, Makoto
Experimental constraints on partial melting under UHT and dry conditions of quartzo-feldspathic rock in the Napier Complex, East Antarctica
title Experimental constraints on partial melting under UHT and dry conditions of quartzo-feldspathic rock in the Napier Complex, East Antarctica
title_full Experimental constraints on partial melting under UHT and dry conditions of quartzo-feldspathic rock in the Napier Complex, East Antarctica
title_fullStr Experimental constraints on partial melting under UHT and dry conditions of quartzo-feldspathic rock in the Napier Complex, East Antarctica
title_full_unstemmed Experimental constraints on partial melting under UHT and dry conditions of quartzo-feldspathic rock in the Napier Complex, East Antarctica
title_short Experimental constraints on partial melting under UHT and dry conditions of quartzo-feldspathic rock in the Napier Complex, East Antarctica
title_sort experimental constraints on partial melting under uht and dry conditions of quartzo-feldspathic rock in the napier complex, east antarctica
topic dry condition
feldspar
melting experiment
Napier Complex
ultrahigh-temperature (UHT) metamorphism
topic_facet dry condition
feldspar
melting experiment
Napier Complex
ultrahigh-temperature (UHT) metamorphism
url https://nipr.repo.nii.ac.jp/record/3084/files/KJ00000044202.pdf
https://doi.org/10.15094/00003084
https://nipr.repo.nii.ac.jp/records/3084