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...
Main Authors: | , |
---|---|
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 |
_version_ | 1829301343885459456 |
---|---|
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 |