Stress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subduction

In continental margins, large-scale, strike-slip fault-systems resulted from oblique subduction commonly exhibit a complex pattern of faulting where major faults define the inland boundary of tectonic slivers that can be detached from the margin. In turn,

Detalles Bibliográficos
Autores: Veloso, E., Gomila, R., González, R., Cembrano, J., Jensen, E., Arancibia, G.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2015
País:Chile
Idioma:inglés
OAI Identifier:oai:repositorio.anid.cl:10533/238143
Acceso en línea:https://hdl.handle.net/10533/238143
Access Level:acceso abierto
id CL_4ddc52cf15608741ec1a088525ca5f5d
oai_identifier_str oai:repositorio.anid.cl:10533/238143
network_acronym_str CL
network_name_str Chile
repository_id_str
spelling Arancibia, G.Jensen, E.Cembrano, J.González, R.Gomila, R.Veloso, E.201510.1016/j.tecto.2015.09.022https://hdl.handle.net/10533/238143http://purl.org/coar/access_right/c_abf2Stress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subductionVeloso, E.Gomila, R.González, R.Cembrano, J.Jensen, E.Arancibia, G.2020-03-11T20:26:55Z2022-07-07T23:45:19Z2020-03-11T20:26:55Z2022-07-07T23:45:19Z2015In continental margins, large-scale, strike-slip fault-systems resulted from oblique subduction commonly exhibit a complex pattern of faulting where major faults define the inland boundary of tectonic slivers that can be detached from the margin. In turn,FONDAPFONDAP1509001315090013virtual::33352-1WOS:000366227800021https://hdl.handle.net/10533/238143eng10.1016/j.tecto.2015.09.022https://doi.org/10.1016/j.tecto.2015.09.022Atribución-NoComercial-SinDerivadas 3.0 Chilehttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/info:eu-repo/semantics/openAccessStress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subductionTectonophysicsArticuloinfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttps://hdl.handle.net/10533/238143FONDAPhttp://purl.org/coar/resource_type/c_2df8fbb1af9f301e-501e-40b1-ba24-0e199f38a218virtual::33352-1af9f301e-501e-40b1-ba24-0e199f38a218virtual::33352-110533/238143oai:repositorio.anid.cl:10533/2381432023-07-24 15:41:36.848https://repositorio.anid.clRepositorio ANIDaletelier@anid.cl
dc.title.none.fl_str_mv Stress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subduction
dc.title.journal.none.fl_str_mv Tectonophysics
title Stress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subduction
spellingShingle Stress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subduction
Veloso, E.
title_short Stress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subduction
title_full Stress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subduction
title_fullStr Stress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subduction
title_full_unstemmed Stress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subduction
title_sort Stress fields recorded on large-scale strike-slip fault systems: Effects on the tectonic evolution of crustal slivers during oblique subduction
dc.creator.none.fl_str_mv Veloso, E.
Gomila, R.
González, R.
Cembrano, J.
Jensen, E.
Arancibia, G.
author Veloso, E.
author_facet Veloso, E.
Gomila, R.
González, R.
Cembrano, J.
Jensen, E.
Arancibia, G.
author_role author
author2 Gomila, R.
González, R.
Cembrano, J.
Jensen, E.
Arancibia, G.
author2_role author
author
author
author
author
description In continental margins, large-scale, strike-slip fault-systems resulted from oblique subduction commonly exhibit a complex pattern of faulting where major faults define the inland boundary of tectonic slivers that can be detached from the margin. In turn,
publishDate 2015
dc.date.issued.none.fl_str_mv 2015
dc.date.accessioned.none.fl_str_mv 2020-03-11T20:26:55Z
2022-07-07T23:45:19Z
dc.date.available.none.fl_str_mv 2020-03-11T20:26:55Z
2022-07-07T23:45:19Z
dc.type.none.fl_str_mv Articulo
dc.type.driver.none.fl_str_mv info:eu-repo/semantics/article
dc.type.openaire.none.fl_str_mv info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.folio.none.fl_str_mv 15090013
15090013
dc.identifier.idwos.none.fl_str_mv WOS:000366227800021
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/10533/238143
identifier_str_mv 15090013
WOS:000366227800021
url https://hdl.handle.net/10533/238143
dc.language.iso.none.fl_str_mv eng
language eng
dc.relation.doi.none.fl_str_mv 10.1016/j.tecto.2015.09.022
dc.relation.uri.none.fl_str_mv https://doi.org/10.1016/j.tecto.2015.09.022
dc.rights.none.fl_str_mv Atribución-NoComercial-SinDerivadas 3.0 Chile
http://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rights.driver.none.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv Atribución-NoComercial-SinDerivadas 3.0 Chile
http://creativecommons.org/licenses/by-nc-nd/3.0/cl/
eu_rights_str_mv openAccess
repository.name.fl_str_mv Repositorio ANID
repository.mail.fl_str_mv aletelier@anid.cl
_version_ 1843518765073956864
score 15.812429

Similares en LA Referencia