Pseudo 3-D modeling of trishear fault-propagation folding
- Autores
- Cristallini, Ernesto Osvaldo; Allmendinger, Richard W.
- Año de publicación
- 2001
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Basement structures, to which trichear fault-propagation models have most successfully been applied, are commonly three-dimensional folds formed at the tip-line of a fault. We present here a 'pseudo-3D' trishear model in which various parameters are permitted to vary along strike and oblique-slip can be modeled. These variations may be combined in an infinite number of ways, facilitating the simulation of many real structures. A thrust changing from blind to emergent can be produced by a change in the slip or propagation-to-slip (P/S) along strike. Folds with forelimbs changing from overturned to upright along strike can be modeled either by changing the slip, P/S or trishear angle. Also some minor folds perpendicular or oblique to the main structure can result from changes in the trishear angle or fault angle along the strike. Models including growth strata show that it is practically impossible to distinguish between growth and pre-growth strata using the map patterns. As a field test, we have modeled the oblique slip East Kaibab monocline, demonstrating a good fit between the field observations and model predictions.
Fil: Cristallini, Ernesto Osvaldo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina
Fil: Allmendinger, Richard W.. Cornell University; Estados Unidos - Materia
-
BASEMENT STRUCTURES
EAST KAIBAB
TRISHEAR FAULT-PROPAGATION FOLDING - 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:11336/93814
Ver los metadatos del registro completo
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Pseudo 3-D modeling of trishear fault-propagation foldingCristallini, Ernesto OsvaldoAllmendinger, Richard W.BASEMENT STRUCTURESEAST KAIBABTRISHEAR FAULT-PROPAGATION FOLDINGhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Basement structures, to which trichear fault-propagation models have most successfully been applied, are commonly three-dimensional folds formed at the tip-line of a fault. We present here a 'pseudo-3D' trishear model in which various parameters are permitted to vary along strike and oblique-slip can be modeled. These variations may be combined in an infinite number of ways, facilitating the simulation of many real structures. A thrust changing from blind to emergent can be produced by a change in the slip or propagation-to-slip (P/S) along strike. Folds with forelimbs changing from overturned to upright along strike can be modeled either by changing the slip, P/S or trishear angle. Also some minor folds perpendicular or oblique to the main structure can result from changes in the trishear angle or fault angle along the strike. Models including growth strata show that it is practically impossible to distinguish between growth and pre-growth strata using the map patterns. As a field test, we have modeled the oblique slip East Kaibab monocline, demonstrating a good fit between the field observations and model predictions.Fil: Cristallini, Ernesto Osvaldo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; ArgentinaFil: Allmendinger, Richard W.. Cornell University; Estados UnidosPergamon-Elsevier Science Ltd2001-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/93814Cristallini, Ernesto Osvaldo; Allmendinger, Richard W.; Pseudo 3-D modeling of trishear fault-propagation folding; Pergamon-Elsevier Science Ltd; Journal Of Structural Geology; 23; 12; 12-2001; 1883-18990191-8141CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0191814101000347info:eu-repo/semantics/altIdentifier/doi/10.1016/S0191-8141(01)00034-7info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:49:52Zoai:ri.conicet.gov.ar:11336/93814instacron: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:34982025-09-03 09:49:53.235CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Pseudo 3-D modeling of trishear fault-propagation folding |
title |
Pseudo 3-D modeling of trishear fault-propagation folding |
spellingShingle |
Pseudo 3-D modeling of trishear fault-propagation folding Cristallini, Ernesto Osvaldo BASEMENT STRUCTURES EAST KAIBAB TRISHEAR FAULT-PROPAGATION FOLDING |
title_short |
Pseudo 3-D modeling of trishear fault-propagation folding |
title_full |
Pseudo 3-D modeling of trishear fault-propagation folding |
title_fullStr |
Pseudo 3-D modeling of trishear fault-propagation folding |
title_full_unstemmed |
Pseudo 3-D modeling of trishear fault-propagation folding |
title_sort |
Pseudo 3-D modeling of trishear fault-propagation folding |
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 |
BASEMENT STRUCTURES EAST KAIBAB TRISHEAR FAULT-PROPAGATION FOLDING |
topic |
BASEMENT STRUCTURES EAST KAIBAB TRISHEAR FAULT-PROPAGATION FOLDING |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Basement structures, to which trichear fault-propagation models have most successfully been applied, are commonly three-dimensional folds formed at the tip-line of a fault. We present here a 'pseudo-3D' trishear model in which various parameters are permitted to vary along strike and oblique-slip can be modeled. These variations may be combined in an infinite number of ways, facilitating the simulation of many real structures. A thrust changing from blind to emergent can be produced by a change in the slip or propagation-to-slip (P/S) along strike. Folds with forelimbs changing from overturned to upright along strike can be modeled either by changing the slip, P/S or trishear angle. Also some minor folds perpendicular or oblique to the main structure can result from changes in the trishear angle or fault angle along the strike. Models including growth strata show that it is practically impossible to distinguish between growth and pre-growth strata using the map patterns. As a field test, we have modeled the oblique slip East Kaibab monocline, demonstrating a good fit between the field observations and model predictions. Fil: Cristallini, Ernesto Osvaldo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Fil: Allmendinger, Richard W.. Cornell University; Estados Unidos |
description |
Basement structures, to which trichear fault-propagation models have most successfully been applied, are commonly three-dimensional folds formed at the tip-line of a fault. We present here a 'pseudo-3D' trishear model in which various parameters are permitted to vary along strike and oblique-slip can be modeled. These variations may be combined in an infinite number of ways, facilitating the simulation of many real structures. A thrust changing from blind to emergent can be produced by a change in the slip or propagation-to-slip (P/S) along strike. Folds with forelimbs changing from overturned to upright along strike can be modeled either by changing the slip, P/S or trishear angle. Also some minor folds perpendicular or oblique to the main structure can result from changes in the trishear angle or fault angle along the strike. Models including growth strata show that it is practically impossible to distinguish between growth and pre-growth strata using the map patterns. As a field test, we have modeled the oblique slip East Kaibab monocline, demonstrating a good fit between the field observations and model predictions. |
publishDate |
2001 |
dc.date.none.fl_str_mv |
2001-12 |
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/11336/93814 Cristallini, Ernesto Osvaldo; Allmendinger, Richard W.; Pseudo 3-D modeling of trishear fault-propagation folding; Pergamon-Elsevier Science Ltd; Journal Of Structural Geology; 23; 12; 12-2001; 1883-1899 0191-8141 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/93814 |
identifier_str_mv |
Cristallini, Ernesto Osvaldo; Allmendinger, Richard W.; Pseudo 3-D modeling of trishear fault-propagation folding; Pergamon-Elsevier Science Ltd; Journal Of Structural Geology; 23; 12; 12-2001; 1883-1899 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/url/https://www.sciencedirect.com/science/article/pii/S0191814101000347 info:eu-repo/semantics/altIdentifier/doi/10.1016/S0191-8141(01)00034-7 |
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) |
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CONICET Digital (CONICET) |
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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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13.13397 |