New constraints on metamorphism in the Highjump Archipelago, East Antarctica
Abstract The age and conditions of metamorphism in the Highjump Archipelago, East Antarctica, are investigated using samples collected during the 1986 Australian Antarctic expedition to the Bunger Hills–Denman Glacier region. In situ U-Pb dating of monazite from three metasedimentary rocks yields ag...
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2016
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Online Access: | http://dx.doi.org/10.1017/s095410201600033x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201600033X |
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crcambridgeupr:10.1017/s095410201600033x 2024-06-23T07:47:21+00:00 New constraints on metamorphism in the Highjump Archipelago, East Antarctica Tucker, Naomi M. Hand, Martin 2016 http://dx.doi.org/10.1017/s095410201600033x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201600033X en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 28, issue 6, page 487-503 ISSN 0954-1020 1365-2079 journal-article 2016 crcambridgeupr https://doi.org/10.1017/s095410201600033x 2024-06-05T04:03:16Z Abstract The age and conditions of metamorphism in the Highjump Archipelago, East Antarctica, are investigated using samples collected during the 1986 Australian Antarctic expedition to the Bunger Hills–Denman Glacier region. In situ U-Pb dating of monazite from three metasedimentary rocks yields ages between c. 1240–1150 Ma and a weighted mean 207 Pb/ 206 Pb age of 1183±8 Ma, consistent with previous constraints on the timing of metamorphism in this region and Stage 2 of the Albany–Fraser Orogeny in south-western Australia. This age is interpreted to date the development of garnet ± sillimanite ± rutile-bearing assemblages that formed at c. 850–950°C and 6–9 kbar. Peak granulite facies metamorphism was followed by decompression, evidenced largely by the partial replacement of garnet by cordierite. These new pressure–temperature determinations suggest that the Highjump Archipelago attained slightly higher temperature and pressure conditions than previously proposed and that the rocks probably experienced a clockwise pressure–temperature evolution. Article in Journal/Newspaper Antarc* Antarctic Antarctic Science Antarctica Denman Glacier East Antarctica Cambridge University Press Antarctic Bunger Hills ENVELOPE(100.883,100.883,-66.167,-66.167) Denman Glacier ENVELOPE(99.417,99.417,-66.750,-66.750) East Antarctica Highjump Archipelago ENVELOPE(100.736,100.736,-66.026,-66.026) Antarctic Science 28 6 487 503 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract The age and conditions of metamorphism in the Highjump Archipelago, East Antarctica, are investigated using samples collected during the 1986 Australian Antarctic expedition to the Bunger Hills–Denman Glacier region. In situ U-Pb dating of monazite from three metasedimentary rocks yields ages between c. 1240–1150 Ma and a weighted mean 207 Pb/ 206 Pb age of 1183±8 Ma, consistent with previous constraints on the timing of metamorphism in this region and Stage 2 of the Albany–Fraser Orogeny in south-western Australia. This age is interpreted to date the development of garnet ± sillimanite ± rutile-bearing assemblages that formed at c. 850–950°C and 6–9 kbar. Peak granulite facies metamorphism was followed by decompression, evidenced largely by the partial replacement of garnet by cordierite. These new pressure–temperature determinations suggest that the Highjump Archipelago attained slightly higher temperature and pressure conditions than previously proposed and that the rocks probably experienced a clockwise pressure–temperature evolution. |
format |
Article in Journal/Newspaper |
author |
Tucker, Naomi M. Hand, Martin |
spellingShingle |
Tucker, Naomi M. Hand, Martin New constraints on metamorphism in the Highjump Archipelago, East Antarctica |
author_facet |
Tucker, Naomi M. Hand, Martin |
author_sort |
Tucker, Naomi M. |
title |
New constraints on metamorphism in the Highjump Archipelago, East Antarctica |
title_short |
New constraints on metamorphism in the Highjump Archipelago, East Antarctica |
title_full |
New constraints on metamorphism in the Highjump Archipelago, East Antarctica |
title_fullStr |
New constraints on metamorphism in the Highjump Archipelago, East Antarctica |
title_full_unstemmed |
New constraints on metamorphism in the Highjump Archipelago, East Antarctica |
title_sort |
new constraints on metamorphism in the highjump archipelago, east antarctica |
publisher |
Cambridge University Press (CUP) |
publishDate |
2016 |
url |
http://dx.doi.org/10.1017/s095410201600033x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201600033X |
long_lat |
ENVELOPE(100.883,100.883,-66.167,-66.167) ENVELOPE(99.417,99.417,-66.750,-66.750) ENVELOPE(100.736,100.736,-66.026,-66.026) |
geographic |
Antarctic Bunger Hills Denman Glacier East Antarctica Highjump Archipelago |
geographic_facet |
Antarctic Bunger Hills Denman Glacier East Antarctica Highjump Archipelago |
genre |
Antarc* Antarctic Antarctic Science Antarctica Denman Glacier East Antarctica |
genre_facet |
Antarc* Antarctic Antarctic Science Antarctica Denman Glacier East Antarctica |
op_source |
Antarctic Science volume 28, issue 6, page 487-503 ISSN 0954-1020 1365-2079 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s095410201600033x |
container_title |
Antarctic Science |
container_volume |
28 |
container_issue |
6 |
container_start_page |
487 |
op_container_end_page |
503 |
_version_ |
1802651442974031872 |