THE EMPLACEMENT PRESSURE OF SYENITE ESTIMATED FROM THE STABILITY FIELD OF AMPHIBOLE FROM THE YAMATO MOUNTAINS, EAST ANTARCTICA
P(論文) T. OBA and K. SHIRAISHI (Proc. NIPR Symp. Antarct. Geosci., 6,72,1993) attempted to estimate the pressure of amphibole-bearing syenites based on the stability field of amphibole in melting experiments. The present study shows improvement over our previous paper. Four hornblende clinopyroxene q...
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Language: | English |
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National Institute of Polar Research
1994
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Online Access: | https://nipr.repo.nii.ac.jp/record/2752/files/KJ00002368382.pdf https://doi.org/10.15094/00002752 https://nipr.repo.nii.ac.jp/records/2752 |
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author | オオバ, タカノブ シライシ, カズユキ OBA, Takanobu SHIRAISHI, Kazuyuki |
author_facet | オオバ, タカノブ シライシ, カズユキ OBA, Takanobu SHIRAISHI, Kazuyuki |
author_sort | オオバ, タカノブ |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) T. OBA and K. SHIRAISHI (Proc. NIPR Symp. Antarct. Geosci., 6,72,1993) attempted to estimate the pressure of amphibole-bearing syenites based on the stability field of amphibole in melting experiments. The present study shows improvement over our previous paper. Four hornblende clinopyroxene quartz syenites, a hornblende clinopyroxene mela-syenite and a hornblende two-pyroxene syenite from the Yamato Mountains were determined under 0.05-0.3 GPa P_<H_2O> in the temperature range 650-900℃, and at the oxygen fugacity of the FMQ buffer. The stability limit curves of amphibole from four syenites (Y556,Y557,Y904 and Y34A) intersect with their solidi at lower pressure than 0.3 GPa. In all syenites except for a mela-syenite (Y405), quartz disappears first, then plagioclase and amphibole in that order with increasing temperature at 0.1 GPa. K-feldspar, in experiments on sample Y405,disappears at lower temperature than amphibole. In experiments on Y405,Y556 and Y904,albite contents in the synthesized K-feldspar slightly increase with increasing temperature below the solidus temperature, whereas the chemical compositions of K-feldspar are constant and around Ab_<45>Or_<55> above the solidus temperature. The chemical compositions of liquids formed by partial melting of syenites are quartz and corundum normative and show the granite minimum composition at 0.1 GPa. They are similar to the chemical compositions of aplitic granites from the southern Yamato Mountains, suggesting that the aplitic granites are low pressure derivatives from the syenites. departmental bulletin paper |
genre | Antarc* Antarctica East Antarctica |
genre_facet | Antarc* Antarctica East Antarctica |
geographic | East Antarctica Yamato |
geographic_facet | East Antarctica Yamato |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00002752 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(35.583,35.583,-71.417,-71.417) |
op_collection_id | ftnipr |
op_doi | https://doi.org/10.15094/00002752 |
op_relation | Proceedings of the NIPR Symposium on Antarctic Geosciences 7 60 68 AA1072335X https://nipr.repo.nii.ac.jp/record/2752/files/KJ00002368382.pdf https://doi.org/10.15094/00002752 https://nipr.repo.nii.ac.jp/records/2752 |
publishDate | 1994 |
publisher | National Institute of Polar Research |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00002752 2025-04-13T14:08:17+00:00 THE EMPLACEMENT PRESSURE OF SYENITE ESTIMATED FROM THE STABILITY FIELD OF AMPHIBOLE FROM THE YAMATO MOUNTAINS, EAST ANTARCTICA オオバ, タカノブ シライシ, カズユキ OBA, Takanobu SHIRAISHI, Kazuyuki 1994-09 application/pdf https://nipr.repo.nii.ac.jp/record/2752/files/KJ00002368382.pdf https://doi.org/10.15094/00002752 https://nipr.repo.nii.ac.jp/records/2752 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Antarctic Geosciences 7 60 68 AA1072335X https://nipr.repo.nii.ac.jp/record/2752/files/KJ00002368382.pdf https://doi.org/10.15094/00002752 https://nipr.repo.nii.ac.jp/records/2752 1994 ftnipr https://doi.org/10.15094/00002752 2025-03-19T10:19:57Z P(論文) T. OBA and K. SHIRAISHI (Proc. NIPR Symp. Antarct. Geosci., 6,72,1993) attempted to estimate the pressure of amphibole-bearing syenites based on the stability field of amphibole in melting experiments. The present study shows improvement over our previous paper. Four hornblende clinopyroxene quartz syenites, a hornblende clinopyroxene mela-syenite and a hornblende two-pyroxene syenite from the Yamato Mountains were determined under 0.05-0.3 GPa P_<H_2O> in the temperature range 650-900℃, and at the oxygen fugacity of the FMQ buffer. The stability limit curves of amphibole from four syenites (Y556,Y557,Y904 and Y34A) intersect with their solidi at lower pressure than 0.3 GPa. In all syenites except for a mela-syenite (Y405), quartz disappears first, then plagioclase and amphibole in that order with increasing temperature at 0.1 GPa. K-feldspar, in experiments on sample Y405,disappears at lower temperature than amphibole. In experiments on Y405,Y556 and Y904,albite contents in the synthesized K-feldspar slightly increase with increasing temperature below the solidus temperature, whereas the chemical compositions of K-feldspar are constant and around Ab_<45>Or_<55> above the solidus temperature. The chemical compositions of liquids formed by partial melting of syenites are quartz and corundum normative and show the granite minimum composition at 0.1 GPa. They are similar to the chemical compositions of aplitic granites from the southern Yamato Mountains, suggesting that the aplitic granites are low pressure derivatives from the syenites. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica National Institute of Polar Research Repository, Japan East Antarctica Yamato ENVELOPE(35.583,35.583,-71.417,-71.417) |
spellingShingle | オオバ, タカノブ シライシ, カズユキ OBA, Takanobu SHIRAISHI, Kazuyuki THE EMPLACEMENT PRESSURE OF SYENITE ESTIMATED FROM THE STABILITY FIELD OF AMPHIBOLE FROM THE YAMATO MOUNTAINS, EAST ANTARCTICA |
title | THE EMPLACEMENT PRESSURE OF SYENITE ESTIMATED FROM THE STABILITY FIELD OF AMPHIBOLE FROM THE YAMATO MOUNTAINS, EAST ANTARCTICA |
title_full | THE EMPLACEMENT PRESSURE OF SYENITE ESTIMATED FROM THE STABILITY FIELD OF AMPHIBOLE FROM THE YAMATO MOUNTAINS, EAST ANTARCTICA |
title_fullStr | THE EMPLACEMENT PRESSURE OF SYENITE ESTIMATED FROM THE STABILITY FIELD OF AMPHIBOLE FROM THE YAMATO MOUNTAINS, EAST ANTARCTICA |
title_full_unstemmed | THE EMPLACEMENT PRESSURE OF SYENITE ESTIMATED FROM THE STABILITY FIELD OF AMPHIBOLE FROM THE YAMATO MOUNTAINS, EAST ANTARCTICA |
title_short | THE EMPLACEMENT PRESSURE OF SYENITE ESTIMATED FROM THE STABILITY FIELD OF AMPHIBOLE FROM THE YAMATO MOUNTAINS, EAST ANTARCTICA |
title_sort | emplacement pressure of syenite estimated from the stability field of amphibole from the yamato mountains, east antarctica |
url | https://nipr.repo.nii.ac.jp/record/2752/files/KJ00002368382.pdf https://doi.org/10.15094/00002752 https://nipr.repo.nii.ac.jp/records/2752 |