Tectonic interactions during rift linkage: insights from analog and numerical experiments

<p>Continental rifts evolve by linkage and interaction of adjacent individual segments. As rift segments propagate, they can cause notable re-orientation of the local stress field so that stress orientations deviate from the regional trend. In return, this stress re-orientation can feed back o...

Full description

Bibliographic Details
Main Authors: T. C. Schmid, S. Brune, A. Glerum, G. Schreurs
Format: Article
Language:English
Published: Copernicus Publications 2023-04-01
Series:Solid Earth
Online Access:https://se.copernicus.org/articles/14/389/2023/se-14-389-2023.pdf
_version_ 1797847510878781440
author T. C. Schmid
S. Brune
S. Brune
A. Glerum
G. Schreurs
author_facet T. C. Schmid
S. Brune
S. Brune
A. Glerum
G. Schreurs
author_sort T. C. Schmid
collection DOAJ
description <p>Continental rifts evolve by linkage and interaction of adjacent individual segments. As rift segments propagate, they can cause notable re-orientation of the local stress field so that stress orientations deviate from the regional trend. In return, this stress re-orientation can feed back on progressive deformation and may ultimately deflect propagating rift segments in an unexpected way. Here, we employ numerical and analog experiments of continental rifting to investigate the interaction between stress re-orientation and segment linkage. Both model types employ crustal-scale two-layer setups wherein pre-existing linear heterogeneities are introduced by mechanical weak seeds. We test various seed configurations to investigate the effect of (i) two competing rift segments that propagate unilaterally, (ii) linkage of two opposingly propagating rift segments, and (iii) the combination of these configurations on stress re-orientation and rift linkage. Both the analog and numerical models show counterintuitive rift deflection of two sub-parallel propagating rift segments competing for linkage with an opposingly propagating segment. The deflection pattern can be explained by means of stress analysis in numerical experiments wherein stress re-orientation occurs locally and propagates across the model domain as rift segments propagate. Major stress re-orientations may occur locally, which means that faults and rift segment trends do not necessarily align perpendicularly to far-field extension directions. Our results show that strain localization and stress re-orientation are closely linked, mutually influence each other, and may be an important factor for rift deflection among competing rift segments as observed in nature.</p>
first_indexed 2024-04-09T18:13:43Z
format Article
id doaj.art-a64ee9ed9e3d4386afa587163b6e7cfc
institution Directory Open Access Journal
issn 1869-9510
1869-9529
language English
last_indexed 2024-04-09T18:13:43Z
publishDate 2023-04-01
publisher Copernicus Publications
record_format Article
series Solid Earth
spelling doaj.art-a64ee9ed9e3d4386afa587163b6e7cfc2023-04-13T11:21:48ZengCopernicus PublicationsSolid Earth1869-95101869-95292023-04-011438940710.5194/se-14-389-2023Tectonic interactions during rift linkage: insights from analog and numerical experimentsT. C. Schmid0S. Brune1S. Brune2A. Glerum3G. Schreurs4Institute of Geological Sciences, University of Bern, Bern, SwitzerlandHelmholtz Centre Potsdam – GFZ German Research Centre for Geosciences, Potsdam, GermanyInstitute of Geosciences, University of Potsdam, Potsdam, GermanyHelmholtz Centre Potsdam – GFZ German Research Centre for Geosciences, Potsdam, GermanyInstitute of Geological Sciences, University of Bern, Bern, Switzerland<p>Continental rifts evolve by linkage and interaction of adjacent individual segments. As rift segments propagate, they can cause notable re-orientation of the local stress field so that stress orientations deviate from the regional trend. In return, this stress re-orientation can feed back on progressive deformation and may ultimately deflect propagating rift segments in an unexpected way. Here, we employ numerical and analog experiments of continental rifting to investigate the interaction between stress re-orientation and segment linkage. Both model types employ crustal-scale two-layer setups wherein pre-existing linear heterogeneities are introduced by mechanical weak seeds. We test various seed configurations to investigate the effect of (i) two competing rift segments that propagate unilaterally, (ii) linkage of two opposingly propagating rift segments, and (iii) the combination of these configurations on stress re-orientation and rift linkage. Both the analog and numerical models show counterintuitive rift deflection of two sub-parallel propagating rift segments competing for linkage with an opposingly propagating segment. The deflection pattern can be explained by means of stress analysis in numerical experiments wherein stress re-orientation occurs locally and propagates across the model domain as rift segments propagate. Major stress re-orientations may occur locally, which means that faults and rift segment trends do not necessarily align perpendicularly to far-field extension directions. Our results show that strain localization and stress re-orientation are closely linked, mutually influence each other, and may be an important factor for rift deflection among competing rift segments as observed in nature.</p>https://se.copernicus.org/articles/14/389/2023/se-14-389-2023.pdf
spellingShingle T. C. Schmid
S. Brune
S. Brune
A. Glerum
G. Schreurs
Tectonic interactions during rift linkage: insights from analog and numerical experiments
Solid Earth
title Tectonic interactions during rift linkage: insights from analog and numerical experiments
title_full Tectonic interactions during rift linkage: insights from analog and numerical experiments
title_fullStr Tectonic interactions during rift linkage: insights from analog and numerical experiments
title_full_unstemmed Tectonic interactions during rift linkage: insights from analog and numerical experiments
title_short Tectonic interactions during rift linkage: insights from analog and numerical experiments
title_sort tectonic interactions during rift linkage insights from analog and numerical experiments
url https://se.copernicus.org/articles/14/389/2023/se-14-389-2023.pdf
work_keys_str_mv AT tcschmid tectonicinteractionsduringriftlinkageinsightsfromanalogandnumericalexperiments
AT sbrune tectonicinteractionsduringriftlinkageinsightsfromanalogandnumericalexperiments
AT sbrune tectonicinteractionsduringriftlinkageinsightsfromanalogandnumericalexperiments
AT aglerum tectonicinteractionsduringriftlinkageinsightsfromanalogandnumericalexperiments
AT gschreurs tectonicinteractionsduringriftlinkageinsightsfromanalogandnumericalexperiments