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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/97626
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3498 |
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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 |
_version_ |
1844613322840735744 |
score |
13.070432 |