SHRIMP U-Pb zircon data from Gjelsvikfjella, Dronning Maud Land, East Antarctica ...
The Maud Belt in Dronning Maud Land (western East Antarctic Craton) preserves a high-grade polyphase tectono-thermal history with two orogenic episodes of Mesoproterozoic (1.2-1.0 Ga) and Neoproterozoic (0.6-0.5 Ga) age. New SHRIMP U-Pb zircon data from southern Gjelsvikfjella in the northeastern pa...
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ftdatacite:10.1594/pangaea.847015 2024-09-15T17:41:50+00:00 SHRIMP U-Pb zircon data from Gjelsvikfjella, Dronning Maud Land, East Antarctica ... Bisnath, Avinash Frimmel, Hartwig E Armstrong, Robert A Board, W S 2006 application/zip https://dx.doi.org/10.1594/pangaea.847015 https://doi.pangaea.de/10.1594/PANGAEA.847015 en eng PANGAEA https://dx.doi.org/10.1016/j.precamres.2006.06.009 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Rock sample Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 article Collection Supplementary Publication Series of Datasets 2006 ftdatacite https://doi.org/10.1594/pangaea.84701510.1016/j.precamres.2006.06.009 2024-08-01T10:57:14Z The Maud Belt in Dronning Maud Land (western East Antarctic Craton) preserves a high-grade polyphase tectono-thermal history with two orogenic episodes of Mesoproterozoic (1.2-1.0 Ga) and Neoproterozoic (0.6-0.5 Ga) age. New SHRIMP U-Pb zircon data from southern Gjelsvikfjella in the northeastern part of the belt make it possible to differentiate between a series of magmatic and metamorphic events. The oldest event recorded is the formation of an extensive 1140-1130 Ma volcanic arc. This was followed by 1104 ± 8 Ma granitoids that might represent, together with so far undated mafic dykes, part of a decompression melting-related bimodal suite that reflects the sub-continental Umkondo igneous event. The first high-grade metamorphism is constrained at 1070 Ma. The metamorphic age data are similar to those obtained from other parts of the Maud Belt, but also from the Namaqua-Natal Belt in South Africa, but the preceding arc formation was diachronous in the two belts. This indicates that the two belts did not ... : Supplement to: Bisnath, Avinash; Frimmel, Hartwig E; Armstrong, Robert A; Board, W S (2006): Tectono-thermal evolution of the Maud Belt: New SHRIMP U–Pb zircon data from Gjelsvikfjella, Dronning Maud Land, East Antarctica. Precambrian Research, 150(1-2), 95-121 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Dronning Maud Land East Antarctica Sea ice DataCite |
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ftdatacite |
language |
English |
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Rock sample Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
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Rock sample Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Bisnath, Avinash Frimmel, Hartwig E Armstrong, Robert A Board, W S SHRIMP U-Pb zircon data from Gjelsvikfjella, Dronning Maud Land, East Antarctica ... |
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Rock sample Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
description |
The Maud Belt in Dronning Maud Land (western East Antarctic Craton) preserves a high-grade polyphase tectono-thermal history with two orogenic episodes of Mesoproterozoic (1.2-1.0 Ga) and Neoproterozoic (0.6-0.5 Ga) age. New SHRIMP U-Pb zircon data from southern Gjelsvikfjella in the northeastern part of the belt make it possible to differentiate between a series of magmatic and metamorphic events. The oldest event recorded is the formation of an extensive 1140-1130 Ma volcanic arc. This was followed by 1104 ± 8 Ma granitoids that might represent, together with so far undated mafic dykes, part of a decompression melting-related bimodal suite that reflects the sub-continental Umkondo igneous event. The first high-grade metamorphism is constrained at 1070 Ma. The metamorphic age data are similar to those obtained from other parts of the Maud Belt, but also from the Namaqua-Natal Belt in South Africa, but the preceding arc formation was diachronous in the two belts. This indicates that the two belts did not ... : Supplement to: Bisnath, Avinash; Frimmel, Hartwig E; Armstrong, Robert A; Board, W S (2006): Tectono-thermal evolution of the Maud Belt: New SHRIMP U–Pb zircon data from Gjelsvikfjella, Dronning Maud Land, East Antarctica. Precambrian Research, 150(1-2), 95-121 ... |
format |
Article in Journal/Newspaper |
author |
Bisnath, Avinash Frimmel, Hartwig E Armstrong, Robert A Board, W S |
author_facet |
Bisnath, Avinash Frimmel, Hartwig E Armstrong, Robert A Board, W S |
author_sort |
Bisnath, Avinash |
title |
SHRIMP U-Pb zircon data from Gjelsvikfjella, Dronning Maud Land, East Antarctica ... |
title_short |
SHRIMP U-Pb zircon data from Gjelsvikfjella, Dronning Maud Land, East Antarctica ... |
title_full |
SHRIMP U-Pb zircon data from Gjelsvikfjella, Dronning Maud Land, East Antarctica ... |
title_fullStr |
SHRIMP U-Pb zircon data from Gjelsvikfjella, Dronning Maud Land, East Antarctica ... |
title_full_unstemmed |
SHRIMP U-Pb zircon data from Gjelsvikfjella, Dronning Maud Land, East Antarctica ... |
title_sort |
shrimp u-pb zircon data from gjelsvikfjella, dronning maud land, east antarctica ... |
publisher |
PANGAEA |
publishDate |
2006 |
url |
https://dx.doi.org/10.1594/pangaea.847015 https://doi.pangaea.de/10.1594/PANGAEA.847015 |
genre |
Antarc* Antarctic Antarctica Dronning Maud Land East Antarctica Sea ice |
genre_facet |
Antarc* Antarctic Antarctica Dronning Maud Land East Antarctica Sea ice |
op_relation |
https://dx.doi.org/10.1016/j.precamres.2006.06.009 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.84701510.1016/j.precamres.2006.06.009 |
_version_ |
1810488118058418176 |