Inversion of accommodation zones in salt-bearing extensional systems: insights from analog modeling

<p>This work uses sandbox analog models to analyze the formation and subsequent inversion of a decoupled extensional system comprised of two segmented half-grabens separated by a diffuse accommodation zone with thick early syn-rift salt. The segmented half-grabens strike perpendicular to the d...

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Main Authors: E. P. Wilson, P. Granado, P. Santolaria, O. Ferrer, J. A. Muñoz
Format: Article
Language:English
Published: Copernicus Publications 2023-07-01
Series:Solid Earth
Online Access:https://se.copernicus.org/articles/14/709/2023/se-14-709-2023.pdf
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author E. P. Wilson
P. Granado
P. Santolaria
O. Ferrer
J. A. Muñoz
author_facet E. P. Wilson
P. Granado
P. Santolaria
O. Ferrer
J. A. Muñoz
author_sort E. P. Wilson
collection DOAJ
description <p>This work uses sandbox analog models to analyze the formation and subsequent inversion of a decoupled extensional system comprised of two segmented half-grabens separated by a diffuse accommodation zone with thick early syn-rift salt. The segmented half-grabens strike perpendicular to the direction of extension and subsequent shortening. Rifting first created a basement topography that was infilled by model salt, followed by a second phase of extension and sedimentation, followed afterwards by inversion. During the second phase of extension, syn-rift syncline minibasins developed above the basement extensional system and extended beyond the confines of the fault blocks. Sedimentary downbuilding and extension initiated the migration of model salt to the basement highs, forming salt anticlines, reactive diapirs, and salt walls perpendicular to the direction of extension, except for along the intervening accommodation zone where a slightly oblique salt anticline developed. Inversion resulted in decoupled cover and basement thrust systems. Thrusts in the cover system nucleated along squeezed salt structures and along primary welds. New primary welds developed where the cover sequence touched down on basement thrust tips due to uplift, salt extrusion, and syn-contractional downbuilding caused by the loading of syn-contractional sedimentation. Model geometries reveal the control imposed by the basement configuration and distribution of salt in the development of a thrust front from the inversion of a salt-bearing extensional system. In 3D, the interaction of salt migrating from adjacent syn-rift basins can modify the expected salt structure geometry, which may in turn influence the location and style of thrust in the cover sequence upon inversion. Results are compared to the Northern Lusitanian Basin, offshore Portugal, and the Isábena area of the South-Central Pyrenees, Spain.</p>
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spelling doaj.art-e64663354a494b2cbdbbe2917d9403572023-07-12T11:43:19ZengCopernicus PublicationsSolid Earth1869-95101869-95292023-07-011470973910.5194/se-14-709-2023Inversion of accommodation zones in salt-bearing extensional systems: insights from analog modelingE. P. WilsonP. GranadoP. SantolariaO. FerrerJ. A. Muñoz<p>This work uses sandbox analog models to analyze the formation and subsequent inversion of a decoupled extensional system comprised of two segmented half-grabens separated by a diffuse accommodation zone with thick early syn-rift salt. The segmented half-grabens strike perpendicular to the direction of extension and subsequent shortening. Rifting first created a basement topography that was infilled by model salt, followed by a second phase of extension and sedimentation, followed afterwards by inversion. During the second phase of extension, syn-rift syncline minibasins developed above the basement extensional system and extended beyond the confines of the fault blocks. Sedimentary downbuilding and extension initiated the migration of model salt to the basement highs, forming salt anticlines, reactive diapirs, and salt walls perpendicular to the direction of extension, except for along the intervening accommodation zone where a slightly oblique salt anticline developed. Inversion resulted in decoupled cover and basement thrust systems. Thrusts in the cover system nucleated along squeezed salt structures and along primary welds. New primary welds developed where the cover sequence touched down on basement thrust tips due to uplift, salt extrusion, and syn-contractional downbuilding caused by the loading of syn-contractional sedimentation. Model geometries reveal the control imposed by the basement configuration and distribution of salt in the development of a thrust front from the inversion of a salt-bearing extensional system. In 3D, the interaction of salt migrating from adjacent syn-rift basins can modify the expected salt structure geometry, which may in turn influence the location and style of thrust in the cover sequence upon inversion. Results are compared to the Northern Lusitanian Basin, offshore Portugal, and the Isábena area of the South-Central Pyrenees, Spain.</p>https://se.copernicus.org/articles/14/709/2023/se-14-709-2023.pdf
spellingShingle E. P. Wilson
P. Granado
P. Santolaria
O. Ferrer
J. A. Muñoz
Inversion of accommodation zones in salt-bearing extensional systems: insights from analog modeling
Solid Earth
title Inversion of accommodation zones in salt-bearing extensional systems: insights from analog modeling
title_full Inversion of accommodation zones in salt-bearing extensional systems: insights from analog modeling
title_fullStr Inversion of accommodation zones in salt-bearing extensional systems: insights from analog modeling
title_full_unstemmed Inversion of accommodation zones in salt-bearing extensional systems: insights from analog modeling
title_short Inversion of accommodation zones in salt-bearing extensional systems: insights from analog modeling
title_sort inversion of accommodation zones in salt bearing extensional systems insights from analog modeling
url https://se.copernicus.org/articles/14/709/2023/se-14-709-2023.pdf
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AT oferrer inversionofaccommodationzonesinsaltbearingextensionalsystemsinsightsfromanalogmodeling
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