Backlimb trishear: A kinematic model for curved folds developed over angular fault bends

Autores
Cristallini, Ernesto Osvaldo; Allmendinger, Richard W.
Año de publicación
2002
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Numerous analog models and some natural examples display smoothly curving backlimb fold hinges over sharp, angular bends in the underlying thrust surface. We present a new kinematic model that can reproduce this geometry by triangular zone focused on the fault bend. The model presupposes incompressible flow in the triangular zone and makes common assumptions about velocities on either side of the fault bend. Either symmetric or asymmetric triangular zones can be defined, with parallel kink folding and similar folding being special cases of the two, respectively, where the apical angle of the triangular zone is zero. The results of the numerical model compare well to analog experiments. The model is conceptually analogous to forelimb at the tip of a propagating fault and hence we refer to it as 'backlimb trishear'.
Fil: Cristallini, Ernesto Osvaldo.
Fil: Allmendinger, R..
Materia
ANGULAR FAULT BENDS
BACKLIMB TRISHEAR
GROWTH STRATA
KINEMATIC MODEL
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/97626

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network_name_str CONICET Digital (CONICET)
spelling Backlimb trishear: A kinematic model for curved folds developed over angular fault bendsCristallini, Ernesto OsvaldoAllmendinger, Richard W.ANGULAR FAULT BENDSBACKLIMB TRISHEARGROWTH STRATAKINEMATIC MODELhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Numerous analog models and some natural examples display smoothly curving backlimb fold hinges over sharp, angular bends in the underlying thrust surface. We present a new kinematic model that can reproduce this geometry by triangular zone focused on the fault bend. The model presupposes incompressible flow in the triangular zone and makes common assumptions about velocities on either side of the fault bend. Either symmetric or asymmetric triangular zones can be defined, with parallel kink folding and similar folding being special cases of the two, respectively, where the apical angle of the triangular zone is zero. The results of the numerical model compare well to analog experiments. The model is conceptually analogous to forelimb at the tip of a propagating fault and hence we refer to it as 'backlimb trishear'.Fil: Cristallini, Ernesto Osvaldo.Fil: Allmendinger, R..Pergamon-Elsevier Science Ltd2002-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/97626Cristallini, Ernesto Osvaldo; Allmendinger, Richard W.; Backlimb trishear: A kinematic model for curved folds developed over angular fault bends; Pergamon-Elsevier Science Ltd; Journal Of Structural Geology; 24; 2; 12-2002; 289-2950191-8141CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/S0191-8141(01)00063-3info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0191814101000633?via%3Dihubinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:41:56Zoai:ri.conicet.gov.ar:11336/97626instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:41:56.399CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Backlimb trishear: A kinematic model for curved folds developed over angular fault bends
title Backlimb trishear: A kinematic model for curved folds developed over angular fault bends
spellingShingle Backlimb trishear: A kinematic model for curved folds developed over angular fault bends
Cristallini, Ernesto Osvaldo
ANGULAR FAULT BENDS
BACKLIMB TRISHEAR
GROWTH STRATA
KINEMATIC MODEL
title_short Backlimb trishear: A kinematic model for curved folds developed over angular fault bends
title_full Backlimb trishear: A kinematic model for curved folds developed over angular fault bends
title_fullStr Backlimb trishear: A kinematic model for curved folds developed over angular fault bends
title_full_unstemmed Backlimb trishear: A kinematic model for curved folds developed over angular fault bends
title_sort Backlimb trishear: A kinematic model for curved folds developed over angular fault bends
dc.creator.none.fl_str_mv Cristallini, Ernesto Osvaldo
Allmendinger, Richard W.
author Cristallini, Ernesto Osvaldo
author_facet Cristallini, Ernesto Osvaldo
Allmendinger, Richard W.
author_role author
author2 Allmendinger, Richard W.
author2_role author
dc.subject.none.fl_str_mv ANGULAR FAULT BENDS
BACKLIMB TRISHEAR
GROWTH STRATA
KINEMATIC MODEL
topic ANGULAR FAULT BENDS
BACKLIMB TRISHEAR
GROWTH STRATA
KINEMATIC MODEL
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Numerous analog models and some natural examples display smoothly curving backlimb fold hinges over sharp, angular bends in the underlying thrust surface. We present a new kinematic model that can reproduce this geometry by triangular zone focused on the fault bend. The model presupposes incompressible flow in the triangular zone and makes common assumptions about velocities on either side of the fault bend. Either symmetric or asymmetric triangular zones can be defined, with parallel kink folding and similar folding being special cases of the two, respectively, where the apical angle of the triangular zone is zero. The results of the numerical model compare well to analog experiments. The model is conceptually analogous to forelimb at the tip of a propagating fault and hence we refer to it as 'backlimb trishear'.
Fil: Cristallini, Ernesto Osvaldo.
Fil: Allmendinger, R..
description Numerous analog models and some natural examples display smoothly curving backlimb fold hinges over sharp, angular bends in the underlying thrust surface. We present a new kinematic model that can reproduce this geometry by triangular zone focused on the fault bend. The model presupposes incompressible flow in the triangular zone and makes common assumptions about velocities on either side of the fault bend. Either symmetric or asymmetric triangular zones can be defined, with parallel kink folding and similar folding being special cases of the two, respectively, where the apical angle of the triangular zone is zero. The results of the numerical model compare well to analog experiments. The model is conceptually analogous to forelimb at the tip of a propagating fault and hence we refer to it as 'backlimb trishear'.
publishDate 2002
dc.date.none.fl_str_mv 2002-12
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/97626
Cristallini, Ernesto Osvaldo; Allmendinger, Richard W.; Backlimb trishear: A kinematic model for curved folds developed over angular fault bends; Pergamon-Elsevier Science Ltd; Journal Of Structural Geology; 24; 2; 12-2002; 289-295
0191-8141
CONICET Digital
CONICET
url http://hdl.handle.net/11336/97626
identifier_str_mv Cristallini, Ernesto Osvaldo; Allmendinger, Richard W.; Backlimb trishear: A kinematic model for curved folds developed over angular fault bends; Pergamon-Elsevier Science Ltd; Journal Of Structural Geology; 24; 2; 12-2002; 289-295
0191-8141
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/S0191-8141(01)00063-3
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0191814101000633?via%3Dihub
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.070432