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
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/120244

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spelling 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).
publishDate 2019
dc.date.none.fl_str_mv 2019-11
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
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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
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language eng
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