Evidence of Paleoproterozoic metamorphism in Vestfold Hills, East Antarctica: Insights from phase equilibria modelling and monazite CHIME dating
The Vestfold Hills sector on the coastal fringe of the Princess Elizabeth Land forms part of an Archean to Paleoproterozoic aged cratonic nucleus of the East Antarctic Shield. A charnockite-granite association from the Mossel Gneiss Group in the northern region of the Vestfold Hills is investigated...
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2023
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ftnipr:oai:nipr.repo.nii.ac.jp:02000368 2024-09-30T14:26:45+00:00 Evidence of Paleoproterozoic metamorphism in Vestfold Hills, East Antarctica: Insights from phase equilibria modelling and monazite CHIME dating Naik Aditya Arora Devsamridhi Pandey Mayuri Pant Naresh Chandra Gupta Rashmi 2023-12-31 https://nipr.repo.nii.ac.jp/records/2000368 eng eng 10.1016/j.polar.2023.101004 https://doi.org/10.1016/j.polar.2023.101004 Polar Science 38 101004 18739652 https://nipr.repo.nii.ac.jp/records/2000368 Vestfold Hills CHIME dating Charnockite Granite Paleoproterozoic NA 2023 ftnipr https://doi.org/10.1016/j.polar.2023.101004 2024-09-17T14:13:03Z The Vestfold Hills sector on the coastal fringe of the Princess Elizabeth Land forms part of an Archean to Paleoproterozoic aged cratonic nucleus of the East Antarctic Shield. A charnockite-granite association from the Mossel Gneiss Group in the northern region of the Vestfold Hills is investigated in this work to characterise the metamorphic-magmatic evolution of the area. Conventional thermometry and phase equilibria modelling indicate that the charnockite formed as a result of ultra-high temperature metamorphism at low-intermediate pressure (∼4 kbar). Phase equilibria modelling, reveals that the melt-integrated charnockite composition is a restitic product of a protolith of quartz diorite composition which underwent isobaric heating (peak temperature up to 960 °C) at 4 kbar pressure followed by anatexis. The anatexis of the quartz diorite protolith also resulted in the formation of the associated granitic melt. U–Th-PbTotal ages obtained from monazites of the granite integrated with CHIME ages extracted using the isochron method indicate an emplacement age of ∼2200 Ma and two younger events are recorded at ∼2000 Ma and ∼1700 Ma. The younger ages are ascribed to the resetting during the emplacement of younger basalt dykes that cross cut the charnockite-granite sequence. Vestfold Hills’ geological correlations with Indian and Australian cratons are discussed considering this new data. journal article Other/Unknown Material Antarc* Antarctic Antarctica East Antarctica Polar Science Polar Science Princess Elizabeth Land National Institute of Polar Research Repository, Japan Antarctic East Antarctica Indian Princess Elizabeth Land ENVELOPE(80.367,80.367,-68.500,-68.500) Vestfold Vestfold Hills Polar Science 38 101004 |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
topic |
Vestfold Hills CHIME dating Charnockite Granite Paleoproterozoic |
spellingShingle |
Vestfold Hills CHIME dating Charnockite Granite Paleoproterozoic Naik Aditya Arora Devsamridhi Pandey Mayuri Pant Naresh Chandra Gupta Rashmi Evidence of Paleoproterozoic metamorphism in Vestfold Hills, East Antarctica: Insights from phase equilibria modelling and monazite CHIME dating |
topic_facet |
Vestfold Hills CHIME dating Charnockite Granite Paleoproterozoic |
description |
The Vestfold Hills sector on the coastal fringe of the Princess Elizabeth Land forms part of an Archean to Paleoproterozoic aged cratonic nucleus of the East Antarctic Shield. A charnockite-granite association from the Mossel Gneiss Group in the northern region of the Vestfold Hills is investigated in this work to characterise the metamorphic-magmatic evolution of the area. Conventional thermometry and phase equilibria modelling indicate that the charnockite formed as a result of ultra-high temperature metamorphism at low-intermediate pressure (∼4 kbar). Phase equilibria modelling, reveals that the melt-integrated charnockite composition is a restitic product of a protolith of quartz diorite composition which underwent isobaric heating (peak temperature up to 960 °C) at 4 kbar pressure followed by anatexis. The anatexis of the quartz diorite protolith also resulted in the formation of the associated granitic melt. U–Th-PbTotal ages obtained from monazites of the granite integrated with CHIME ages extracted using the isochron method indicate an emplacement age of ∼2200 Ma and two younger events are recorded at ∼2000 Ma and ∼1700 Ma. The younger ages are ascribed to the resetting during the emplacement of younger basalt dykes that cross cut the charnockite-granite sequence. Vestfold Hills’ geological correlations with Indian and Australian cratons are discussed considering this new data. journal article |
format |
Other/Unknown Material |
author |
Naik Aditya Arora Devsamridhi Pandey Mayuri Pant Naresh Chandra Gupta Rashmi |
author_facet |
Naik Aditya Arora Devsamridhi Pandey Mayuri Pant Naresh Chandra Gupta Rashmi |
author_sort |
Naik Aditya |
title |
Evidence of Paleoproterozoic metamorphism in Vestfold Hills, East Antarctica: Insights from phase equilibria modelling and monazite CHIME dating |
title_short |
Evidence of Paleoproterozoic metamorphism in Vestfold Hills, East Antarctica: Insights from phase equilibria modelling and monazite CHIME dating |
title_full |
Evidence of Paleoproterozoic metamorphism in Vestfold Hills, East Antarctica: Insights from phase equilibria modelling and monazite CHIME dating |
title_fullStr |
Evidence of Paleoproterozoic metamorphism in Vestfold Hills, East Antarctica: Insights from phase equilibria modelling and monazite CHIME dating |
title_full_unstemmed |
Evidence of Paleoproterozoic metamorphism in Vestfold Hills, East Antarctica: Insights from phase equilibria modelling and monazite CHIME dating |
title_sort |
evidence of paleoproterozoic metamorphism in vestfold hills, east antarctica: insights from phase equilibria modelling and monazite chime dating |
publishDate |
2023 |
url |
https://nipr.repo.nii.ac.jp/records/2000368 |
long_lat |
ENVELOPE(80.367,80.367,-68.500,-68.500) |
geographic |
Antarctic East Antarctica Indian Princess Elizabeth Land Vestfold Vestfold Hills |
geographic_facet |
Antarctic East Antarctica Indian Princess Elizabeth Land Vestfold Vestfold Hills |
genre |
Antarc* Antarctic Antarctica East Antarctica Polar Science Polar Science Princess Elizabeth Land |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica Polar Science Polar Science Princess Elizabeth Land |
op_relation |
10.1016/j.polar.2023.101004 https://doi.org/10.1016/j.polar.2023.101004 Polar Science 38 101004 18739652 https://nipr.repo.nii.ac.jp/records/2000368 |
op_doi |
https://doi.org/10.1016/j.polar.2023.101004 |
container_title |
Polar Science |
container_volume |
38 |
container_start_page |
101004 |
_version_ |
1811632866611691520 |