Outboard Onset of Ross Orogen Magmatism and Subsequent Igneous and Metamorphic Cooling Linked to Slab Rollback during Late-Stage Gondwana Assembly ...
Changes in magmatism and sedimentation along the late Neoproterozoic-early Paleozoic Ross orogenic belt in Antarctica have been linked to the cessation of convergence along the Mozambique belt during the assembly of East-West Gondwana. However, these interpretations are non-unique and are based, in...
Main Authors: | , , , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
ETH Zurich
2023
|
Subjects: | |
Online Access: | https://dx.doi.org/10.3929/ethz-b-000610928 http://hdl.handle.net/20.500.11850/610928 |
id |
ftdatacite:10.3929/ethz-b-000610928 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.3929/ethz-b-000610928 2024-04-28T07:57:37+00:00 Outboard Onset of Ross Orogen Magmatism and Subsequent Igneous and Metamorphic Cooling Linked to Slab Rollback during Late-Stage Gondwana Assembly ... Paulsen, Timothy Encarnación, John Grunow, Anne Benowitz, Jeffrey Layer, Paul Deering, Chad Sliwinski, Jakub 2023 application/pdf https://dx.doi.org/10.3929/ethz-b-000610928 http://hdl.handle.net/20.500.11850/610928 en eng ETH Zurich 40Ar/39Ar cooling magmatism zircon trace elements slab rollback Ross orogen Antarctica Gondwana article-journal Text ScholarlyArticle Journal Article 2023 ftdatacite https://doi.org/10.3929/ethz-b-000610928 2024-04-02T12:32:08Z Changes in magmatism and sedimentation along the late Neoproterozoic-early Paleozoic Ross orogenic belt in Antarctica have been linked to the cessation of convergence along the Mozambique belt during the assembly of East-West Gondwana. However, these interpretations are non-unique and are based, in part, on limited thermochronological data sets spread out along large sectors of the East Antarctic margin. We report new 40Ar/39Ar hornblende, muscovite, and biotite age data for plutonic (n = 13) and metasedimentary (n = 3) samples from the Shackleton–Liv Glacier sector of the Queen Maud Mountains in Antarctica. Cumulative 40Ar/39Ar age data show polymodal age peaks (510 Ma, 491 Ma, 475 Ma) that lag peaks in U-Pb igneous crystallization ages, suggesting igneous and metamorphic cooling following magmatism within the region. The 40Ar/39Ar ages are similar to ages in other sectors of the Ross orogen, but younger than detrital mineral 40Ar/39Ar cooling ages indicative of older magmatism and cooling of unexposed ... : Geosciences, 13 (4) ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Liv Glacier DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
40Ar/39Ar cooling magmatism zircon trace elements slab rollback Ross orogen Antarctica Gondwana |
spellingShingle |
40Ar/39Ar cooling magmatism zircon trace elements slab rollback Ross orogen Antarctica Gondwana Paulsen, Timothy Encarnación, John Grunow, Anne Benowitz, Jeffrey Layer, Paul Deering, Chad Sliwinski, Jakub Outboard Onset of Ross Orogen Magmatism and Subsequent Igneous and Metamorphic Cooling Linked to Slab Rollback during Late-Stage Gondwana Assembly ... |
topic_facet |
40Ar/39Ar cooling magmatism zircon trace elements slab rollback Ross orogen Antarctica Gondwana |
description |
Changes in magmatism and sedimentation along the late Neoproterozoic-early Paleozoic Ross orogenic belt in Antarctica have been linked to the cessation of convergence along the Mozambique belt during the assembly of East-West Gondwana. However, these interpretations are non-unique and are based, in part, on limited thermochronological data sets spread out along large sectors of the East Antarctic margin. We report new 40Ar/39Ar hornblende, muscovite, and biotite age data for plutonic (n = 13) and metasedimentary (n = 3) samples from the Shackleton–Liv Glacier sector of the Queen Maud Mountains in Antarctica. Cumulative 40Ar/39Ar age data show polymodal age peaks (510 Ma, 491 Ma, 475 Ma) that lag peaks in U-Pb igneous crystallization ages, suggesting igneous and metamorphic cooling following magmatism within the region. The 40Ar/39Ar ages are similar to ages in other sectors of the Ross orogen, but younger than detrital mineral 40Ar/39Ar cooling ages indicative of older magmatism and cooling of unexposed ... : Geosciences, 13 (4) ... |
format |
Article in Journal/Newspaper |
author |
Paulsen, Timothy Encarnación, John Grunow, Anne Benowitz, Jeffrey Layer, Paul Deering, Chad Sliwinski, Jakub |
author_facet |
Paulsen, Timothy Encarnación, John Grunow, Anne Benowitz, Jeffrey Layer, Paul Deering, Chad Sliwinski, Jakub |
author_sort |
Paulsen, Timothy |
title |
Outboard Onset of Ross Orogen Magmatism and Subsequent Igneous and Metamorphic Cooling Linked to Slab Rollback during Late-Stage Gondwana Assembly ... |
title_short |
Outboard Onset of Ross Orogen Magmatism and Subsequent Igneous and Metamorphic Cooling Linked to Slab Rollback during Late-Stage Gondwana Assembly ... |
title_full |
Outboard Onset of Ross Orogen Magmatism and Subsequent Igneous and Metamorphic Cooling Linked to Slab Rollback during Late-Stage Gondwana Assembly ... |
title_fullStr |
Outboard Onset of Ross Orogen Magmatism and Subsequent Igneous and Metamorphic Cooling Linked to Slab Rollback during Late-Stage Gondwana Assembly ... |
title_full_unstemmed |
Outboard Onset of Ross Orogen Magmatism and Subsequent Igneous and Metamorphic Cooling Linked to Slab Rollback during Late-Stage Gondwana Assembly ... |
title_sort |
outboard onset of ross orogen magmatism and subsequent igneous and metamorphic cooling linked to slab rollback during late-stage gondwana assembly ... |
publisher |
ETH Zurich |
publishDate |
2023 |
url |
https://dx.doi.org/10.3929/ethz-b-000610928 http://hdl.handle.net/20.500.11850/610928 |
genre |
Antarc* Antarctic Antarctica Liv Glacier |
genre_facet |
Antarc* Antarctic Antarctica Liv Glacier |
op_doi |
https://doi.org/10.3929/ethz-b-000610928 |
_version_ |
1797589469321232384 |