MONAZITE AGES BY THE CHEMICAL Th-U-TOTAL Pb ISOCHRON METHOD FOR PELITIC GNEISSES FROM THE EASTERN SØR RONDANE MOUNTAINS, EAST ANTARCTICA
Chemical Th-U-total Pb isochron (CHIME) ages were determined with an electron microprobe analyzer on 14 to 24 monazite grains in three garnet-biotite gneisses collected from separate outcrops in the eastern part of the Sør Rondane Mountains, East Antarctica. On the basis of geologic and petrologic s...
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Department of Earth Sciences, Faculty of Science, Okayama University
1996
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ftnipr:oai:nipr.repo.nii.ac.jp:00002823 2023-05-15T13:49:00+02:00 MONAZITE AGES BY THE CHEMICAL Th-U-TOTAL Pb ISOCHRON METHOD FOR PELITIC GNEISSES FROM THE EASTERN SØR RONDANE MOUNTAINS, EAST ANTARCTICA アサミ マサオ スズキ カズヒロ アダチ マモル Masao ASAMI Kazuhiro SUZUKI Mamoru ADACHI 1996-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2823 http://id.nii.ac.jp/1291/00002823/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2823&item_no=1&attribute_id=18&file_no=1 en eng Department of Earth Sciences, Faculty of Science, Okayama University Department of Earth and Planetary Sciences, School of Science, Nagoya University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2823 http://id.nii.ac.jp/1291/00002823/ AA1072335X Proceedings of the NIPR Symposium on Antarctic Geosciences, 9, 49-64(1996-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2823&item_no=1&attribute_id=18&file_no=1 CHIME age monazite Cambrian granulite facies Sør Rondane Mountains Departmental Bulletin Paper P(論文) 1996 ftnipr 2022-11-26T19:42:17Z Chemical Th-U-total Pb isochron (CHIME) ages were determined with an electron microprobe analyzer on 14 to 24 monazite grains in three garnet-biotite gneisses collected from separate outcrops in the eastern part of the Sør Rondane Mountains, East Antarctica. On the basis of geologic and petrologic studies, investigators have inferred a two-stage metamorphic history for the Sør Rondane : (1) an earlier regional granulite-facies event inferred from U-Pb zircon and Rb-Sr and Sm-Nd whole rock data to be ∿1000Ma in age, and (2) an amphibolite-facies overprint inferred to be ∿500Ma in age. PbO-ThO_2^* plots based on ThO_2,UO_2 and PbO contents of monazites yield a well-defined isochron for each gneiss, although both matrix grains in all gneiss samples and inclusions in garnet and pyrrhotite grains in a sample were analyzed. The isochrons give 536,534 and 534 Ma ages, indicating a single crystallization age (~535Ma) for the monazites. This age is in good agreement with the ~500Ma age currently assigned to the amphibolite-facies overprint. However, the high Pb retentivity reported for monazite, along with textural and mineralogical characteristics of the samples, constrains assignment of the monazite age to the granulite-facies metamorphism rather than to retrograde recrystallization. Our ~535Ma ages give rise to a possibility of further westward extension of a Cambrian orogenic belt recently reported from the Lützow-Holm and Yamato-Belgica Complexes, where a similar succession of metamorphic and plutonic activities has been recognized. Report Antarc* Antarctica East Antarctica National Institute of Polar Research Repository, Japan East Antarctica Yamato ENVELOPE(35.583,35.583,-71.417,-71.417) Sør-Rondane ENVELOPE(25.000,25.000,-72.000,-72.000) Sør Rondane Mountains ENVELOPE(25.000,25.000,-72.000,-72.000) |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
topic |
CHIME age monazite Cambrian granulite facies Sør Rondane Mountains |
spellingShingle |
CHIME age monazite Cambrian granulite facies Sør Rondane Mountains アサミ マサオ スズキ カズヒロ アダチ マモル Masao ASAMI Kazuhiro SUZUKI Mamoru ADACHI MONAZITE AGES BY THE CHEMICAL Th-U-TOTAL Pb ISOCHRON METHOD FOR PELITIC GNEISSES FROM THE EASTERN SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
topic_facet |
CHIME age monazite Cambrian granulite facies Sør Rondane Mountains |
description |
Chemical Th-U-total Pb isochron (CHIME) ages were determined with an electron microprobe analyzer on 14 to 24 monazite grains in three garnet-biotite gneisses collected from separate outcrops in the eastern part of the Sør Rondane Mountains, East Antarctica. On the basis of geologic and petrologic studies, investigators have inferred a two-stage metamorphic history for the Sør Rondane : (1) an earlier regional granulite-facies event inferred from U-Pb zircon and Rb-Sr and Sm-Nd whole rock data to be ∿1000Ma in age, and (2) an amphibolite-facies overprint inferred to be ∿500Ma in age. PbO-ThO_2^* plots based on ThO_2,UO_2 and PbO contents of monazites yield a well-defined isochron for each gneiss, although both matrix grains in all gneiss samples and inclusions in garnet and pyrrhotite grains in a sample were analyzed. The isochrons give 536,534 and 534 Ma ages, indicating a single crystallization age (~535Ma) for the monazites. This age is in good agreement with the ~500Ma age currently assigned to the amphibolite-facies overprint. However, the high Pb retentivity reported for monazite, along with textural and mineralogical characteristics of the samples, constrains assignment of the monazite age to the granulite-facies metamorphism rather than to retrograde recrystallization. Our ~535Ma ages give rise to a possibility of further westward extension of a Cambrian orogenic belt recently reported from the Lützow-Holm and Yamato-Belgica Complexes, where a similar succession of metamorphic and plutonic activities has been recognized. |
format |
Report |
author |
アサミ マサオ スズキ カズヒロ アダチ マモル Masao ASAMI Kazuhiro SUZUKI Mamoru ADACHI |
author_facet |
アサミ マサオ スズキ カズヒロ アダチ マモル Masao ASAMI Kazuhiro SUZUKI Mamoru ADACHI |
author_sort |
アサミ マサオ |
title |
MONAZITE AGES BY THE CHEMICAL Th-U-TOTAL Pb ISOCHRON METHOD FOR PELITIC GNEISSES FROM THE EASTERN SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
title_short |
MONAZITE AGES BY THE CHEMICAL Th-U-TOTAL Pb ISOCHRON METHOD FOR PELITIC GNEISSES FROM THE EASTERN SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
title_full |
MONAZITE AGES BY THE CHEMICAL Th-U-TOTAL Pb ISOCHRON METHOD FOR PELITIC GNEISSES FROM THE EASTERN SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
title_fullStr |
MONAZITE AGES BY THE CHEMICAL Th-U-TOTAL Pb ISOCHRON METHOD FOR PELITIC GNEISSES FROM THE EASTERN SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
title_full_unstemmed |
MONAZITE AGES BY THE CHEMICAL Th-U-TOTAL Pb ISOCHRON METHOD FOR PELITIC GNEISSES FROM THE EASTERN SØR RONDANE MOUNTAINS, EAST ANTARCTICA |
title_sort |
monazite ages by the chemical th-u-total pb isochron method for pelitic gneisses from the eastern sør rondane mountains, east antarctica |
publisher |
Department of Earth Sciences, Faculty of Science, Okayama University |
publishDate |
1996 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2823 http://id.nii.ac.jp/1291/00002823/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2823&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(35.583,35.583,-71.417,-71.417) ENVELOPE(25.000,25.000,-72.000,-72.000) ENVELOPE(25.000,25.000,-72.000,-72.000) |
geographic |
East Antarctica Yamato Sør-Rondane Sør Rondane Mountains |
geographic_facet |
East Antarctica Yamato Sør-Rondane Sør Rondane Mountains |
genre |
Antarc* Antarctica East Antarctica |
genre_facet |
Antarc* Antarctica East Antarctica |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2823 http://id.nii.ac.jp/1291/00002823/ AA1072335X Proceedings of the NIPR Symposium on Antarctic Geosciences, 9, 49-64(1996-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2823&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250317734739968 |