Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Reparto de la deformación"'
Autor:
Díaz Azpiroz, Manuel, Barcos, Leticia, Expósito, Inmaculada, Jiménez Bonilla, Alejandro, Balanyá, Juan Carlos, Fernández Rodríguez, Carlos|||0000-0001-5135-7972
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
Complex strain partitioning patterns are very common in the continental crust. They are often related to the kinematics of three-dimensional deformations and hence, can be analysed using transpression models. In this work, the strain partitioning pat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::446d286f9eedc8e0e47ca2cf85e2597d
http://hdl.handle.net/10272/10630
http://hdl.handle.net/10272/10630
El desarrollo de zonas transpresivas normalmente está relacionado con límites de placas de convergencia oblicua. La deformación dentro de estas zonas presenta un alto grado de reparto cuando se localizan en la corteza superior. El Macizo del Torca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::d0a7e6a8666badbac6fce891f256430d
Autor:
Jiménez Bonilla, Alejandro, Balanyá, Juan Carlos, Expósito, Inmaculada, Crespo Blanc, Ana, Torvela, Taija, Díaz Azpiroz, Manuel, Barcos, Leticia
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The External Zones of migrating orogenic arcs can be deformed as fold-and-thrust belts where the advance of the deformation front toward the foreland is contemporary to the arc-lengthening. The Sierra de Cabra, in the Central Betics, is made up of Su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::717ea2708ffd9d322f1f0b4375c682d1
http://hdl.handle.net/10272/13571
http://hdl.handle.net/10272/13571
Autor:
Barcos Murcia, Leticia
Programa de Doctorado en Estudios Medioambientales
Transpressive high-strain zones are common features in the lateral parts of orogenic arcs where oblique convergence usually occurs. The strain within these zones is highly partitioned when they
Transpressive high-strain zones are common features in the lateral parts of orogenic arcs where oblique convergence usually occurs. The strain within these zones is highly partitioned when they
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3034::3b3fa0373b1c7e54ae00eefd7656f895
https://hdl.handle.net/10433/2139
https://hdl.handle.net/10433/2139
Autor:
Barcos, Leticia, Jiménez Bonilla, Alejandro, Expósito, Inmaculada, Balanyá, Juan Carlos, Díaz Azpiroz, Manuel
The eastern end of the Torcal Shear Zone (TSZ) is made up of two structural domains that accommodate variable proportions of the strain partitioning associated to the TSZ dextral transpressive deformation. The Sierra de las Cabras Domain is a dextral
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::49887734540905e266c9b4f09aae6a56
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
El desarrollo de zonas transpresivas normalmente está relacionado con límites de placas de convergencia oblicua. La deformación dentro de estas zonas presenta un alto grado de reparto cuando se localizan en la corteza superior. El Macizo del Torca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::d0a7e6a8666badbac6fce891f256430d
http://hdl.handle.net/10272/7347
http://hdl.handle.net/10272/7347
Publikováno v:
Journal of Iberian Geology; September 2017, Vol. 43 Issue: 3 p497-518, 22p
Autor:
RODRIGUEZ-VALDIVIA, MARCELO, URDAY-URDAY, EDWIN JULIO, ELIAS PANTIGOSO-GÓMEZ, EDWIN, ANDRADE-TACCA, CESAR AUGUSTO
Publikováno v:
Revista Iberoamericana de Ingeniería Mecánica; oct2022, Vol. 26 Issue 2, p47-59, 13p
Autor:
Jiménez Bonilla, Alejandro, Balanyá, Juan Carlos, Expósito, Inmaculada, Crespo Blanc, Ana, Torvela, Taija, Díaz Azpiroz, Manuel, Barcos, Leticia
The External Zones of migrating orogenic arcs can be deformed as fold-and-thrust belts where the advance of the deformation front toward the foreland is contemporary to the arc-lengthening. The Sierra de Cabra, in the Central Betics, is made up of Su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1388::717ea2708ffd9d322f1f0b4375c682d1
https://hdl.handle.net/10272/13571
https://hdl.handle.net/10272/13571
Autor:
Barcos, Leticia, Jiménez Bonilla, Alejandro, Expósito, Inmaculada, Balanyá, Juan Carlos, Díaz Azpiroz, Manuel
Publikováno v:
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
instname
The eastern end of the Torcal Shear Zone (TSZ) is made up of two structural domains that accommodate variable proportions of the strain partitioning associated to the TSZ dextral transpressive deformation. The Sierra de las Cabras Domain is a dextral
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=RECOLECTA___::49887734540905e266c9b4f09aae6a56
http://hdl.handle.net/10272/10629
http://hdl.handle.net/10272/10629