Coupling between fluids and rock deformation in the continental crust : Preface
- Autores
- Japas, Maria Silvia; Oriolo, Sebastián; Samuel, Vinod
- Año de publicación
- 2019
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Fluids are essential and widespread components of the Earth crust. They regulate the main process of mass and energy transport, conditioning the geochemical and geophysical evolution of thecrust (Bredehoeft and Norton, 1990) and, consequently, its properties and mechanical behavior. The coupling between fluids, rock deformation, and heat are crucial engines for plate tectonics, playing a leading role in the rheology and evolution of the lithosphere (e.g. Jamtveit et al., 2000; Kennedy and van Soest, 2007; Thompson,2010; Miller, 2013; Yardley and Bodnar, 2014; Hirauchi et al., 2016; Menzies et al., 2016; Plümper et al., 2017; Vizán et al., 2017). They strongly contribute to the viability of the Wilson cycle, since cyclic redistribution of fluids guarantees the survival of a dynamic Earth (Fyfe, 1985, 1997; Bercovici, 1998; Ribeiro, 2002; Bercovici et al.,2015, chap. 7.07; Tajima et al., 2015). The influence exerted by fluids on rock deformation (and vice versa) is significant, regardless of the tectonic setting (e.g. Oliver, 1986; McCaig et al., 2000; Doubre and Peltzer, 2007; Naganjaneyulu and Santosh, 2011; Suppe, 2014; Beaudoin et al., 2014; Williams et al., 2015; Zheng et al., 2016), crustal level (e.g. Sibson, 1994; Cosgrove, 1995; Cox, 2002; Hobbs and Ord, 2018; Papeschi et al., 2018) and scale (e.g. Carter et al., 1990; Holyoke and Kronenberg, 2013; Tajima et al., 2015).
Fil: Japas, Maria Silvia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Oriolo, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Samuel, Vinod. Yonsei University; Corea del Sur - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/120244
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Coupling between fluids and rock deformation in the continental crust : PrefaceJapas, Maria SilviaOriolo, SebastiánSamuel, Vinodhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Fluids are essential and widespread components of the Earth crust. They regulate the main process of mass and energy transport, conditioning the geochemical and geophysical evolution of thecrust (Bredehoeft and Norton, 1990) and, consequently, its properties and mechanical behavior. The coupling between fluids, rock deformation, and heat are crucial engines for plate tectonics, playing a leading role in the rheology and evolution of the lithosphere (e.g. Jamtveit et al., 2000; Kennedy and van Soest, 2007; Thompson,2010; Miller, 2013; Yardley and Bodnar, 2014; Hirauchi et al., 2016; Menzies et al., 2016; Plümper et al., 2017; Vizán et al., 2017). They strongly contribute to the viability of the Wilson cycle, since cyclic redistribution of fluids guarantees the survival of a dynamic Earth (Fyfe, 1985, 1997; Bercovici, 1998; Ribeiro, 2002; Bercovici et al.,2015, chap. 7.07; Tajima et al., 2015). The influence exerted by fluids on rock deformation (and vice versa) is significant, regardless of the tectonic setting (e.g. Oliver, 1986; McCaig et al., 2000; Doubre and Peltzer, 2007; Naganjaneyulu and Santosh, 2011; Suppe, 2014; Beaudoin et al., 2014; Williams et al., 2015; Zheng et al., 2016), crustal level (e.g. Sibson, 1994; Cosgrove, 1995; Cox, 2002; Hobbs and Ord, 2018; Papeschi et al., 2018) and scale (e.g. Carter et al., 1990; Holyoke and Kronenberg, 2013; Tajima et al., 2015).Fil: Japas, Maria Silvia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Oriolo, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Samuel, Vinod. Yonsei University; Corea del SurElsevier2019-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/120244Japas, Maria Silvia; Oriolo, Sebastián; Samuel, Vinod; Coupling between fluids and rock deformation in the continental crust : Preface; Elsevier; Geoscience Frontiers; 10; 6; 11-2019; 2085-20921674-9871CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.gsf.2019.07.001info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1674987119301252info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:49:31Zoai:ri.conicet.gov.ar:11336/120244instacron: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 09:49:31.707CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Coupling between fluids and rock deformation in the continental crust : Preface |
title |
Coupling between fluids and rock deformation in the continental crust : Preface |
spellingShingle |
Coupling between fluids and rock deformation in the continental crust : Preface Japas, Maria Silvia |
title_short |
Coupling between fluids and rock deformation in the continental crust : Preface |
title_full |
Coupling between fluids and rock deformation in the continental crust : Preface |
title_fullStr |
Coupling between fluids and rock deformation in the continental crust : Preface |
title_full_unstemmed |
Coupling between fluids and rock deformation in the continental crust : Preface |
title_sort |
Coupling between fluids and rock deformation in the continental crust : Preface |
dc.creator.none.fl_str_mv |
Japas, Maria Silvia Oriolo, Sebastián Samuel, Vinod |
author |
Japas, Maria Silvia |
author_facet |
Japas, Maria Silvia Oriolo, Sebastián Samuel, Vinod |
author_role |
author |
author2 |
Oriolo, Sebastián Samuel, Vinod |
author2_role |
author author |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Fluids are essential and widespread components of the Earth crust. They regulate the main process of mass and energy transport, conditioning the geochemical and geophysical evolution of thecrust (Bredehoeft and Norton, 1990) and, consequently, its properties and mechanical behavior. The coupling between fluids, rock deformation, and heat are crucial engines for plate tectonics, playing a leading role in the rheology and evolution of the lithosphere (e.g. Jamtveit et al., 2000; Kennedy and van Soest, 2007; Thompson,2010; Miller, 2013; Yardley and Bodnar, 2014; Hirauchi et al., 2016; Menzies et al., 2016; Plümper et al., 2017; Vizán et al., 2017). They strongly contribute to the viability of the Wilson cycle, since cyclic redistribution of fluids guarantees the survival of a dynamic Earth (Fyfe, 1985, 1997; Bercovici, 1998; Ribeiro, 2002; Bercovici et al.,2015, chap. 7.07; Tajima et al., 2015). The influence exerted by fluids on rock deformation (and vice versa) is significant, regardless of the tectonic setting (e.g. Oliver, 1986; McCaig et al., 2000; Doubre and Peltzer, 2007; Naganjaneyulu and Santosh, 2011; Suppe, 2014; Beaudoin et al., 2014; Williams et al., 2015; Zheng et al., 2016), crustal level (e.g. Sibson, 1994; Cosgrove, 1995; Cox, 2002; Hobbs and Ord, 2018; Papeschi et al., 2018) and scale (e.g. Carter et al., 1990; Holyoke and Kronenberg, 2013; Tajima et al., 2015). Fil: Japas, Maria Silvia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina Fil: Oriolo, Sebastián. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina Fil: Samuel, Vinod. Yonsei University; Corea del Sur |
description |
Fluids are essential and widespread components of the Earth crust. They regulate the main process of mass and energy transport, conditioning the geochemical and geophysical evolution of thecrust (Bredehoeft and Norton, 1990) and, consequently, its properties and mechanical behavior. The coupling between fluids, rock deformation, and heat are crucial engines for plate tectonics, playing a leading role in the rheology and evolution of the lithosphere (e.g. Jamtveit et al., 2000; Kennedy and van Soest, 2007; Thompson,2010; Miller, 2013; Yardley and Bodnar, 2014; Hirauchi et al., 2016; Menzies et al., 2016; Plümper et al., 2017; Vizán et al., 2017). They strongly contribute to the viability of the Wilson cycle, since cyclic redistribution of fluids guarantees the survival of a dynamic Earth (Fyfe, 1985, 1997; Bercovici, 1998; Ribeiro, 2002; Bercovici et al.,2015, chap. 7.07; Tajima et al., 2015). The influence exerted by fluids on rock deformation (and vice versa) is significant, regardless of the tectonic setting (e.g. Oliver, 1986; McCaig et al., 2000; Doubre and Peltzer, 2007; Naganjaneyulu and Santosh, 2011; Suppe, 2014; Beaudoin et al., 2014; Williams et al., 2015; Zheng et al., 2016), crustal level (e.g. Sibson, 1994; Cosgrove, 1995; Cox, 2002; Hobbs and Ord, 2018; Papeschi et al., 2018) and scale (e.g. Carter et al., 1990; Holyoke and Kronenberg, 2013; Tajima et al., 2015). |
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2019 |
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2019-11 |
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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/11336/120244 Japas, Maria Silvia; Oriolo, Sebastián; Samuel, Vinod; Coupling between fluids and rock deformation in the continental crust : Preface; Elsevier; Geoscience Frontiers; 10; 6; 11-2019; 2085-2092 1674-9871 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/120244 |
identifier_str_mv |
Japas, Maria Silvia; Oriolo, Sebastián; Samuel, Vinod; Coupling between fluids and rock deformation in the continental crust : Preface; Elsevier; Geoscience Frontiers; 10; 6; 11-2019; 2085-2092 1674-9871 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
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info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gsf.2019.07.001 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1674987119301252 |
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Elsevier |
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Elsevier |
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