The post-orogenic evolution of the Northeast Greenland Caledonides constrained from apatite fission track analysis and inverse geodynamic modelling

International audience We present new apatite !ssion track (AFT) data from the Northeast Greenland passive margin, between 75.8 and 81°N, where elevations reach over 1000 m and no signs of magmatism related to the opening of the North Atlantic exist. The AFT ages are old, ranging from just less than...

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Published in:Tectonophysics
Main Authors: Pedersen, V., K., Nielsen, Soren-Bom, Gallagher, Kerry
Other Authors: Terre, Temps, Traçage, Géosciences Rennes (GR), Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR), Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)-Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR), Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2012
Subjects:
Online Access:https://insu.hal.science/insu-00714401
https://doi.org/10.1016/j.tecto.2012.01.018
id ftunivrennes1hal:oai:HAL:insu-00714401v1
record_format openpolar
institution Open Polar
collection Université de Rennes 1: Publications scientifiques (HAL)
op_collection_id ftunivrennes1hal
language English
topic Northeast Greenland
Fission track analysis
Passive margins
Topography
Erosion
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
spellingShingle Northeast Greenland
Fission track analysis
Passive margins
Topography
Erosion
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Pedersen, V., K.
Nielsen, Soren-Bom
Gallagher, Kerry
The post-orogenic evolution of the Northeast Greenland Caledonides constrained from apatite fission track analysis and inverse geodynamic modelling
topic_facet Northeast Greenland
Fission track analysis
Passive margins
Topography
Erosion
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
description International audience We present new apatite !ssion track (AFT) data from the Northeast Greenland passive margin, between 75.8 and 81°N, where elevations reach over 1000 m and no signs of magmatism related to the opening of the North Atlantic exist. The AFT ages are old, ranging from just less than 200 Ma up to more than 350 Ma, and the length distributions are predominantly narrow unimodal, with c-axis projected mean track lengths between 13.3 and 15.0 !m. The passive margin of Northeast Greenland differs from other studied passive margins in terms of AFT age trends, as we observe no correlation with elevation or characteristic trends relative to mean track length. Using these new data and inverse geodynamic modelling, we constrain the evolution in the area since the orogenic collapse of the Caledonides. Exhumation histories are inferred using a uniform stretching model, incorporating variable rates of erosion or deposition, and thermal histories are found by solving the onedimensional transient conduction-advection heat equation. These thermal histories are used with the observed !ssion track data to constrain acceptable strain rate histories and exhumation paths. The results suggest that rifting has been focused mainly in the now offshore regions since ~300 Ma, or in minor local areas onshore, not affecting the sampled areas signi!cantly. The present-day high topography is therefore suggested simply to represent remnants of the original Caledonian topography, modi!ed during early rifting and, other than the "exural isostatic response to erosional unloading, we !nd no need for introducing post-rift related uplift mechanisms.
author2 Terre, Temps, Traçage
Géosciences Rennes (GR)
Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR)
Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)-Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR)
Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Pedersen, V., K.
Nielsen, Soren-Bom
Gallagher, Kerry
author_facet Pedersen, V., K.
Nielsen, Soren-Bom
Gallagher, Kerry
author_sort Pedersen, V., K.
title The post-orogenic evolution of the Northeast Greenland Caledonides constrained from apatite fission track analysis and inverse geodynamic modelling
title_short The post-orogenic evolution of the Northeast Greenland Caledonides constrained from apatite fission track analysis and inverse geodynamic modelling
title_full The post-orogenic evolution of the Northeast Greenland Caledonides constrained from apatite fission track analysis and inverse geodynamic modelling
title_fullStr The post-orogenic evolution of the Northeast Greenland Caledonides constrained from apatite fission track analysis and inverse geodynamic modelling
title_full_unstemmed The post-orogenic evolution of the Northeast Greenland Caledonides constrained from apatite fission track analysis and inverse geodynamic modelling
title_sort post-orogenic evolution of the northeast greenland caledonides constrained from apatite fission track analysis and inverse geodynamic modelling
publisher HAL CCSD
publishDate 2012
url https://insu.hal.science/insu-00714401
https://doi.org/10.1016/j.tecto.2012.01.018
geographic Greenland
geographic_facet Greenland
genre Greenland
North Atlantic
genre_facet Greenland
North Atlantic
op_source ISSN: 0040-1951
EISSN: 1879-3266
Tectonophysics
https://insu.hal.science/insu-00714401
Tectonophysics, 2012, 530-531, pp.318-330. ⟨10.1016/j.tecto.2012.01.018⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2012.01.018
insu-00714401
https://insu.hal.science/insu-00714401
doi:10.1016/j.tecto.2012.01.018
op_doi https://doi.org/10.1016/j.tecto.2012.01.018
container_title Tectonophysics
container_volume 530-531
container_start_page 318
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spelling ftunivrennes1hal:oai:HAL:insu-00714401v1 2024-02-11T10:04:14+01:00 The post-orogenic evolution of the Northeast Greenland Caledonides constrained from apatite fission track analysis and inverse geodynamic modelling Pedersen, V., K. Nielsen, Soren-Bom Gallagher, Kerry Terre, Temps, Traçage Géosciences Rennes (GR) Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR) Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)-Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR) Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS) 2012 https://insu.hal.science/insu-00714401 https://doi.org/10.1016/j.tecto.2012.01.018 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2012.01.018 insu-00714401 https://insu.hal.science/insu-00714401 doi:10.1016/j.tecto.2012.01.018 ISSN: 0040-1951 EISSN: 1879-3266 Tectonophysics https://insu.hal.science/insu-00714401 Tectonophysics, 2012, 530-531, pp.318-330. ⟨10.1016/j.tecto.2012.01.018⟩ Northeast Greenland Fission track analysis Passive margins Topography Erosion [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2012 ftunivrennes1hal https://doi.org/10.1016/j.tecto.2012.01.018 2024-01-23T23:45:29Z International audience We present new apatite !ssion track (AFT) data from the Northeast Greenland passive margin, between 75.8 and 81°N, where elevations reach over 1000 m and no signs of magmatism related to the opening of the North Atlantic exist. The AFT ages are old, ranging from just less than 200 Ma up to more than 350 Ma, and the length distributions are predominantly narrow unimodal, with c-axis projected mean track lengths between 13.3 and 15.0 !m. The passive margin of Northeast Greenland differs from other studied passive margins in terms of AFT age trends, as we observe no correlation with elevation or characteristic trends relative to mean track length. Using these new data and inverse geodynamic modelling, we constrain the evolution in the area since the orogenic collapse of the Caledonides. Exhumation histories are inferred using a uniform stretching model, incorporating variable rates of erosion or deposition, and thermal histories are found by solving the onedimensional transient conduction-advection heat equation. These thermal histories are used with the observed !ssion track data to constrain acceptable strain rate histories and exhumation paths. The results suggest that rifting has been focused mainly in the now offshore regions since ~300 Ma, or in minor local areas onshore, not affecting the sampled areas signi!cantly. The present-day high topography is therefore suggested simply to represent remnants of the original Caledonian topography, modi!ed during early rifting and, other than the "exural isostatic response to erosional unloading, we !nd no need for introducing post-rift related uplift mechanisms. Article in Journal/Newspaper Greenland North Atlantic Université de Rennes 1: Publications scientifiques (HAL) Greenland Tectonophysics 530-531 318 330