Thermochronological ( 40 Ar/ 39 Ar) evidence of Early Palaeozoic basin inversion within the southern Prince Charles Mountains, East Antarctica: implications for East Gondwana

40 Ar/ 39 Ar systematics within metasedimentary rocks exposed in the southern Prince Charles Mountains, East Antarctica, were thermally reset during a period of Early Palaeozoic (between 524 ± 1 Ma and 486 ± 2 Ma) orogenesis. This event affected three temporally distinct (Archaean to Neoproterozoic)...

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Main Authors: Phillips, Glen, Wilson, Christopher J.L., Phillips, David, Szczepanski, Stan K.
Format: Dataset
Language:unknown
Published: Geological Society of London 2016
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.3454400.v1
https://geolsoc.figshare.com/articles/dataset/Thermochronological_sup_40_sup_Ar_sup_39_sup_Ar_evidence_of_Early_Palaeozoic_basin_inversion_within_the_southern_Prince_Charles_Mountains_East_Antarctica_implications___for_East_Gondwana/3454400/1
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spelling ftdatacite:10.6084/m9.figshare.3454400.v1 2023-05-15T13:34:28+02:00 Thermochronological ( 40 Ar/ 39 Ar) evidence of Early Palaeozoic basin inversion within the southern Prince Charles Mountains, East Antarctica: implications for East Gondwana Phillips, Glen Wilson, Christopher J.L. Phillips, David Szczepanski, Stan K. 2016 https://dx.doi.org/10.6084/m9.figshare.3454400.v1 https://geolsoc.figshare.com/articles/dataset/Thermochronological_sup_40_sup_Ar_sup_39_sup_Ar_evidence_of_Early_Palaeozoic_basin_inversion_within_the_southern_Prince_Charles_Mountains_East_Antarctica_implications___for_East_Gondwana/3454400/1 unknown Geological Society of London https://dx.doi.org/10.1144/0016-76492006-073 https://dx.doi.org/10.6084/m9.figshare.3454400 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Geology FOS Earth and related environmental sciences dataset Dataset 2016 ftdatacite https://doi.org/10.6084/m9.figshare.3454400.v1 https://doi.org/10.1144/0016-76492006-073 https://doi.org/10.6084/m9.figshare.3454400 2021-11-05T12:55:41Z 40 Ar/ 39 Ar systematics within metasedimentary rocks exposed in the southern Prince Charles Mountains, East Antarctica, were thermally reset during a period of Early Palaeozoic (between 524 ± 1 Ma and 486 ± 2 Ma) orogenesis. This event affected three temporally distinct (Archaean to Neoproterozoic) stratigraphic levels that are now exposed in the upper crust. In the structural record, evidence of orogenesis during Early Palaeozoic times is preserved as late-stage, subvertical mylonite zones in the Archaean orthogneiss–metasedimentary basement and thin-skinned folding and thrusting of the overlying Neoproterozoic metasedimentary rocks. Synchronous cooling ages, contrasting structural styles and similar peak metamorphic conditions are interpreted as reflecting basement-involved thin-skinned deformation that was the result of inversion of a Neoproterozoic basin. The presence of pre-existing crustal heterogeneities is the mechanism that localized Early Palaeozoic orogenesis within the region. This interpretation differs from previous models that attribute Early Palaeozoic orogenesis within the southern Prince Charles Mountains to a collisional tectonic setting. An Early Palaeozoic intra-cratonic setting for the region suggests that amalgamation between India and Antarctica was likely to have occurred prior to the final construction of Gondwana. Dataset Antarc* Antarctica East Antarctica Prince Charles Mountains DataCite Metadata Store (German National Library of Science and Technology) East Antarctica Prince Charles Mountains ENVELOPE(67.246,67.246,-71.427,-71.427)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Geology
FOS Earth and related environmental sciences
spellingShingle Geology
FOS Earth and related environmental sciences
Phillips, Glen
Wilson, Christopher J.L.
Phillips, David
Szczepanski, Stan K.
Thermochronological ( 40 Ar/ 39 Ar) evidence of Early Palaeozoic basin inversion within the southern Prince Charles Mountains, East Antarctica: implications for East Gondwana
topic_facet Geology
FOS Earth and related environmental sciences
description 40 Ar/ 39 Ar systematics within metasedimentary rocks exposed in the southern Prince Charles Mountains, East Antarctica, were thermally reset during a period of Early Palaeozoic (between 524 ± 1 Ma and 486 ± 2 Ma) orogenesis. This event affected three temporally distinct (Archaean to Neoproterozoic) stratigraphic levels that are now exposed in the upper crust. In the structural record, evidence of orogenesis during Early Palaeozoic times is preserved as late-stage, subvertical mylonite zones in the Archaean orthogneiss–metasedimentary basement and thin-skinned folding and thrusting of the overlying Neoproterozoic metasedimentary rocks. Synchronous cooling ages, contrasting structural styles and similar peak metamorphic conditions are interpreted as reflecting basement-involved thin-skinned deformation that was the result of inversion of a Neoproterozoic basin. The presence of pre-existing crustal heterogeneities is the mechanism that localized Early Palaeozoic orogenesis within the region. This interpretation differs from previous models that attribute Early Palaeozoic orogenesis within the southern Prince Charles Mountains to a collisional tectonic setting. An Early Palaeozoic intra-cratonic setting for the region suggests that amalgamation between India and Antarctica was likely to have occurred prior to the final construction of Gondwana.
format Dataset
author Phillips, Glen
Wilson, Christopher J.L.
Phillips, David
Szczepanski, Stan K.
author_facet Phillips, Glen
Wilson, Christopher J.L.
Phillips, David
Szczepanski, Stan K.
author_sort Phillips, Glen
title Thermochronological ( 40 Ar/ 39 Ar) evidence of Early Palaeozoic basin inversion within the southern Prince Charles Mountains, East Antarctica: implications for East Gondwana
title_short Thermochronological ( 40 Ar/ 39 Ar) evidence of Early Palaeozoic basin inversion within the southern Prince Charles Mountains, East Antarctica: implications for East Gondwana
title_full Thermochronological ( 40 Ar/ 39 Ar) evidence of Early Palaeozoic basin inversion within the southern Prince Charles Mountains, East Antarctica: implications for East Gondwana
title_fullStr Thermochronological ( 40 Ar/ 39 Ar) evidence of Early Palaeozoic basin inversion within the southern Prince Charles Mountains, East Antarctica: implications for East Gondwana
title_full_unstemmed Thermochronological ( 40 Ar/ 39 Ar) evidence of Early Palaeozoic basin inversion within the southern Prince Charles Mountains, East Antarctica: implications for East Gondwana
title_sort thermochronological ( 40 ar/ 39 ar) evidence of early palaeozoic basin inversion within the southern prince charles mountains, east antarctica: implications for east gondwana
publisher Geological Society of London
publishDate 2016
url https://dx.doi.org/10.6084/m9.figshare.3454400.v1
https://geolsoc.figshare.com/articles/dataset/Thermochronological_sup_40_sup_Ar_sup_39_sup_Ar_evidence_of_Early_Palaeozoic_basin_inversion_within_the_southern_Prince_Charles_Mountains_East_Antarctica_implications___for_East_Gondwana/3454400/1
long_lat ENVELOPE(67.246,67.246,-71.427,-71.427)
geographic East Antarctica
Prince Charles Mountains
geographic_facet East Antarctica
Prince Charles Mountains
genre Antarc*
Antarctica
East Antarctica
Prince Charles Mountains
genre_facet Antarc*
Antarctica
East Antarctica
Prince Charles Mountains
op_relation https://dx.doi.org/10.1144/0016-76492006-073
https://dx.doi.org/10.6084/m9.figshare.3454400
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.6084/m9.figshare.3454400.v1
https://doi.org/10.1144/0016-76492006-073
https://doi.org/10.6084/m9.figshare.3454400
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