AMMONIUM CONTENT OF BIOTITES FROM GRANITIC AND METAMORPHIC ROCKS IN THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA

P(論文) Ammonium content of biotites from granitic and metamorphic rocks in the Sør Rondane Mountains in East Antarctica has been determined in order to examine the difference in the NH_4^+ content of biotites among six granite types. Ammonium content of biotites ranges from 12 to 23ppm (average, 18pp...

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Main Authors: タイノショウ, ヨシアキ, タカハシ, ユウヘイ, オサナイ, ヤスヒト, ツチヤ, ノリヨシ, TAINOSHO, Yoshiaki, TAKAHASHI, Yuhei, OSANAI, Yasuhito, TSUCHIYA, Noriyoshi
Language:English
Published: National Institute of Polar Research 1991
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/2692/files/KJ00002368275.pdf
https://doi.org/10.15094/00002692
https://nipr.repo.nii.ac.jp/records/2692
_version_ 1829311392349421568
author タイノショウ, ヨシアキ
タカハシ, ユウヘイ
オサナイ, ヤスヒト
ツチヤ, ノリヨシ
TAINOSHO, Yoshiaki
TAKAHASHI, Yuhei
OSANAI, Yasuhito
TSUCHIYA, Noriyoshi
author_facet タイノショウ, ヨシアキ
タカハシ, ユウヘイ
オサナイ, ヤスヒト
ツチヤ, ノリヨシ
TAINOSHO, Yoshiaki
TAKAHASHI, Yuhei
OSANAI, Yasuhito
TSUCHIYA, Noriyoshi
author_sort タイノショウ, ヨシアキ
collection National Institute of Polar Research Repository, Japan
description P(論文) Ammonium content of biotites from granitic and metamorphic rocks in the Sør Rondane Mountains in East Antarctica has been determined in order to examine the difference in the NH_4^+ content of biotites among six granite types. Ammonium content of biotites ranges from 12 to 23ppm (average, 18ppm) in the migmatitic granite, 23 to 80ppm in the foliated granite (average, 46ppm), 22 to 86ppm (average, 66ppm) in the massive granite with migmatitic margin, 11 to 66ppm (average, 42ppm) in the discordant granite, 28 to 106ppm (average, 67ppm) in the granite sheet and dyke, 76 to 109ppm (average, 92ppm) in the small granodiorite bodies, and 25 to 142 ppm (average, 52ppm) in the metamorphic rocks. High NH_4^+ content found in biotites from the small granodiorite bodies is probably due to a result of the interaction between the granitic magma and surrounding metamorphic rocks. Biotites from the migmatitic granite have lowest NH_4^+ content in granitic rocks analyzed. The fact is in discord with the field evidence. The very low NH_4^+ content in biotite from the Nils Larsen tonalite is in good accordance with the view postulated from petrochemical data that granitic magma of this tonalite was directly derived from the melting of subducted oceanic crust or the overlying mantle. In metamorphic rocks, the low NH_4^+ content in biotites is probably due to liberation of NH_4^+ from the rocks during high grade metamorphism (granulite facies). departmental bulletin paper
genre Antarc*
Antarctica
East Antarctica
genre_facet Antarc*
Antarctica
East Antarctica
geographic East Antarctica
Nils
Sør-Rondane
Sør Rondane Mountains
Nils Larsen
geographic_facet East Antarctica
Nils
Sør-Rondane
Sør Rondane Mountains
Nils Larsen
id ftnipr:oai:nipr.repo.nii.ac.jp:00002692
institution Open Polar
language English
long_lat ENVELOPE(48.017,48.017,-68.067,-68.067)
ENVELOPE(25.000,25.000,-72.000,-72.000)
ENVELOPE(25.000,25.000,-72.000,-72.000)
ENVELOPE(23.167,23.167,-72.300,-72.300)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00002692
op_relation Proceedings of the NIPR Symposium on Antarctic Geosciences
5
112
121
AA1072335X
https://nipr.repo.nii.ac.jp/record/2692/files/KJ00002368275.pdf
https://doi.org/10.15094/00002692
https://nipr.repo.nii.ac.jp/records/2692
publishDate 1991
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00002692 2025-04-13T14:08:17+00:00 AMMONIUM CONTENT OF BIOTITES FROM GRANITIC AND METAMORPHIC ROCKS IN THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA タイノショウ, ヨシアキ タカハシ, ユウヘイ オサナイ, ヤスヒト ツチヤ, ノリヨシ TAINOSHO, Yoshiaki TAKAHASHI, Yuhei OSANAI, Yasuhito TSUCHIYA, Noriyoshi 1991-09 application/pdf https://nipr.repo.nii.ac.jp/record/2692/files/KJ00002368275.pdf https://doi.org/10.15094/00002692 https://nipr.repo.nii.ac.jp/records/2692 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Antarctic Geosciences 5 112 121 AA1072335X https://nipr.repo.nii.ac.jp/record/2692/files/KJ00002368275.pdf https://doi.org/10.15094/00002692 https://nipr.repo.nii.ac.jp/records/2692 1991 ftnipr https://doi.org/10.15094/00002692 2025-03-19T10:19:57Z P(論文) Ammonium content of biotites from granitic and metamorphic rocks in the Sør Rondane Mountains in East Antarctica has been determined in order to examine the difference in the NH_4^+ content of biotites among six granite types. Ammonium content of biotites ranges from 12 to 23ppm (average, 18ppm) in the migmatitic granite, 23 to 80ppm in the foliated granite (average, 46ppm), 22 to 86ppm (average, 66ppm) in the massive granite with migmatitic margin, 11 to 66ppm (average, 42ppm) in the discordant granite, 28 to 106ppm (average, 67ppm) in the granite sheet and dyke, 76 to 109ppm (average, 92ppm) in the small granodiorite bodies, and 25 to 142 ppm (average, 52ppm) in the metamorphic rocks. High NH_4^+ content found in biotites from the small granodiorite bodies is probably due to a result of the interaction between the granitic magma and surrounding metamorphic rocks. Biotites from the migmatitic granite have lowest NH_4^+ content in granitic rocks analyzed. The fact is in discord with the field evidence. The very low NH_4^+ content in biotite from the Nils Larsen tonalite is in good accordance with the view postulated from petrochemical data that granitic magma of this tonalite was directly derived from the melting of subducted oceanic crust or the overlying mantle. In metamorphic rocks, the low NH_4^+ content in biotites is probably due to liberation of NH_4^+ from the rocks during high grade metamorphism (granulite facies). departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica National Institute of Polar Research Repository, Japan East Antarctica Nils ENVELOPE(48.017,48.017,-68.067,-68.067) Sør-Rondane ENVELOPE(25.000,25.000,-72.000,-72.000) Sør Rondane Mountains ENVELOPE(25.000,25.000,-72.000,-72.000) Nils Larsen ENVELOPE(23.167,23.167,-72.300,-72.300)
spellingShingle タイノショウ, ヨシアキ
タカハシ, ユウヘイ
オサナイ, ヤスヒト
ツチヤ, ノリヨシ
TAINOSHO, Yoshiaki
TAKAHASHI, Yuhei
OSANAI, Yasuhito
TSUCHIYA, Noriyoshi
AMMONIUM CONTENT OF BIOTITES FROM GRANITIC AND METAMORPHIC ROCKS IN THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title AMMONIUM CONTENT OF BIOTITES FROM GRANITIC AND METAMORPHIC ROCKS IN THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_full AMMONIUM CONTENT OF BIOTITES FROM GRANITIC AND METAMORPHIC ROCKS IN THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_fullStr AMMONIUM CONTENT OF BIOTITES FROM GRANITIC AND METAMORPHIC ROCKS IN THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_full_unstemmed AMMONIUM CONTENT OF BIOTITES FROM GRANITIC AND METAMORPHIC ROCKS IN THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_short AMMONIUM CONTENT OF BIOTITES FROM GRANITIC AND METAMORPHIC ROCKS IN THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_sort ammonium content of biotites from granitic and metamorphic rocks in the sør rondane mountains, east antarctica
url https://nipr.repo.nii.ac.jp/record/2692/files/KJ00002368275.pdf
https://doi.org/10.15094/00002692
https://nipr.repo.nii.ac.jp/records/2692