Rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere

Observations from rifted margins reveal that significant structural and crustal variability develops through the process of continental extension and breakup. While a clear link exists between distinct margin structural domains and specific phases of rifting, the origin of strong segmentation along...

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Main Authors: Gouiza, M, Naliboff, J
Format: Article in Journal/Newspaper
Language:English
Published: Nature Research 2021
Subjects:
Online Access:https://eprints.whiterose.ac.uk/182511/
https://eprints.whiterose.ac.uk/182511/6/s41467-021-24945-5.pdf
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spelling ftleedsuniv:oai:eprints.whiterose.ac.uk:182511 2023-05-15T17:06:09+02:00 Rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere Gouiza, M Naliboff, J 2021-08-02 text https://eprints.whiterose.ac.uk/182511/ https://eprints.whiterose.ac.uk/182511/6/s41467-021-24945-5.pdf en eng Nature Research https://eprints.whiterose.ac.uk/182511/6/s41467-021-24945-5.pdf Gouiza, M orcid.org/0000-0001-5438-2698 and Naliboff, J (2021) Rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere. Nature Communications, 12 (1). 4653. ISSN 2041-1723 cc_by_4 CC-BY Article NonPeerReviewed 2021 ftleedsuniv 2023-01-30T22:44:01Z Observations from rifted margins reveal that significant structural and crustal variability develops through the process of continental extension and breakup. While a clear link exists between distinct margin structural domains and specific phases of rifting, the origin of strong segmentation along the length of margins remains relatively ambiguous and may reflect multiple competing factors. Given that rifting frequently initiates on heterogenous basements with a complex tectonic history, the role of structural inheritance and shear zone reactivation is frequently examined. However, the link between large-scale variations in lithospheric structure and rheology and 3-D rifted margin geometries remains relatively unconstrained. Here, we use 3-D thermo-mechanical simulations of continental rifting, constrained by observations from the Labrador Sea, to unravel the effects of inherited variable lithospheric properties on margin segmentation. The modelling results demonstrate that variations in the initial crustal and lithospheric thickness, composition, and rheology produce sharp gradients in rifted margin width, the timing of breakup and its magmatic budget, leading to strong margin segmentation. Article in Journal/Newspaper Labrador Sea White Rose Research Online (Universities of Leeds, Sheffield & York)
institution Open Polar
collection White Rose Research Online (Universities of Leeds, Sheffield & York)
op_collection_id ftleedsuniv
language English
description Observations from rifted margins reveal that significant structural and crustal variability develops through the process of continental extension and breakup. While a clear link exists between distinct margin structural domains and specific phases of rifting, the origin of strong segmentation along the length of margins remains relatively ambiguous and may reflect multiple competing factors. Given that rifting frequently initiates on heterogenous basements with a complex tectonic history, the role of structural inheritance and shear zone reactivation is frequently examined. However, the link between large-scale variations in lithospheric structure and rheology and 3-D rifted margin geometries remains relatively unconstrained. Here, we use 3-D thermo-mechanical simulations of continental rifting, constrained by observations from the Labrador Sea, to unravel the effects of inherited variable lithospheric properties on margin segmentation. The modelling results demonstrate that variations in the initial crustal and lithospheric thickness, composition, and rheology produce sharp gradients in rifted margin width, the timing of breakup and its magmatic budget, leading to strong margin segmentation.
format Article in Journal/Newspaper
author Gouiza, M
Naliboff, J
spellingShingle Gouiza, M
Naliboff, J
Rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere
author_facet Gouiza, M
Naliboff, J
author_sort Gouiza, M
title Rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere
title_short Rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere
title_full Rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere
title_fullStr Rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere
title_full_unstemmed Rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere
title_sort rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere
publisher Nature Research
publishDate 2021
url https://eprints.whiterose.ac.uk/182511/
https://eprints.whiterose.ac.uk/182511/6/s41467-021-24945-5.pdf
genre Labrador Sea
genre_facet Labrador Sea
op_relation https://eprints.whiterose.ac.uk/182511/6/s41467-021-24945-5.pdf
Gouiza, M orcid.org/0000-0001-5438-2698 and Naliboff, J (2021) Rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere. Nature Communications, 12 (1). 4653. ISSN 2041-1723
op_rights cc_by_4
op_rightsnorm CC-BY
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