Cross-strike structures controlling magmatism emplacement in a flat-slab setting (Precordillera, Central Andes of Argentina)

Detailed structural, kinematic and geophysical data on the foreland of the Pampean flatslab segment (Hualilán area, Andean Precordillera of Argentina) have shown that cross-strike structures have had an important role in the evolution of this Andean segment since Miocene times. These structures repr...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Oriolo, Sebastián, Japas, Maria Silvia, Cristallini, Ernesto Osvaldo
Publicado: 2014
Materias:
crustal structure
emplacement
foreland basin
magmatism
Miocene
orogeny
Pliocene
slab
Argentina
Precordillera
Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03058719_v394_n1_p113_Oriolo
http://hdl.handle.net/20.500.12110/paper_03058719_v394_n1_p113_Oriolo
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires
id paper:paper_03058719_v394_n1_p113_Oriolo
record_format dspace
spelling paper:paper_03058719_v394_n1_p113_Oriolo2023-06-08T15:30:57Z Cross-strike structures controlling magmatism emplacement in a flat-slab setting (Precordillera, Central Andes of Argentina) Oriolo, Sebastián Japas, Maria Silvia Cristallini, Ernesto Osvaldo crustal structure emplacement foreland basin magmatism Miocene orogeny Pliocene slab Argentina Precordillera Detailed structural, kinematic and geophysical data on the foreland of the Pampean flatslab segment (Hualilán area, Andean Precordillera of Argentina) have shown that cross-strike structures have had an important role in the evolution of this Andean segment since Miocene times. These structures represent pre-existing crustal fabrics reactivated during the Andean orogeny and could have controlled the emplacement of the Miocene arc-magmatism migrating into foreland due to the flattening of the slab. Likewise, kinematic results obtained for these structures support a similar stress frame to that obtained elsewhere in the Precordillera but showing different motions as a consequence of their high obliquity to the orogen trend. Moreover, they record a reorientation of kinematic axes during Late Miocene-Pliocene times. © The Geological Society of London 2014. Fil:Oriolo, S. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Japas, M.S. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Cristallini, E.O. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2014 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03058719_v394_n1_p113_Oriolo http://hdl.handle.net/20.500.12110/paper_03058719_v394_n1_p113_Oriolo
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic crustal structure
emplacement
foreland basin
magmatism
Miocene
orogeny
Pliocene
slab
Argentina
Precordillera
spellingShingle crustal structure
emplacement
foreland basin
magmatism
Miocene
orogeny
Pliocene
slab
Argentina
Precordillera
Oriolo, Sebastián
Japas, Maria Silvia
Cristallini, Ernesto Osvaldo
Cross-strike structures controlling magmatism emplacement in a flat-slab setting (Precordillera, Central Andes of Argentina)
topic_facet crustal structure
emplacement
foreland basin
magmatism
Miocene
orogeny
Pliocene
slab
Argentina
Precordillera
description Detailed structural, kinematic and geophysical data on the foreland of the Pampean flatslab segment (Hualilán area, Andean Precordillera of Argentina) have shown that cross-strike structures have had an important role in the evolution of this Andean segment since Miocene times. These structures represent pre-existing crustal fabrics reactivated during the Andean orogeny and could have controlled the emplacement of the Miocene arc-magmatism migrating into foreland due to the flattening of the slab. Likewise, kinematic results obtained for these structures support a similar stress frame to that obtained elsewhere in the Precordillera but showing different motions as a consequence of their high obliquity to the orogen trend. Moreover, they record a reorientation of kinematic axes during Late Miocene-Pliocene times. © The Geological Society of London 2014.
author Oriolo, Sebastián
Japas, Maria Silvia
Cristallini, Ernesto Osvaldo
author_facet Oriolo, Sebastián
Japas, Maria Silvia
Cristallini, Ernesto Osvaldo
author_sort Oriolo, Sebastián
title Cross-strike structures controlling magmatism emplacement in a flat-slab setting (Precordillera, Central Andes of Argentina)
title_short Cross-strike structures controlling magmatism emplacement in a flat-slab setting (Precordillera, Central Andes of Argentina)
title_full Cross-strike structures controlling magmatism emplacement in a flat-slab setting (Precordillera, Central Andes of Argentina)
title_fullStr Cross-strike structures controlling magmatism emplacement in a flat-slab setting (Precordillera, Central Andes of Argentina)
title_full_unstemmed Cross-strike structures controlling magmatism emplacement in a flat-slab setting (Precordillera, Central Andes of Argentina)
title_sort cross-strike structures controlling magmatism emplacement in a flat-slab setting (precordillera, central andes of argentina)
publishDate 2014
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03058719_v394_n1_p113_Oriolo
http://hdl.handle.net/20.500.12110/paper_03058719_v394_n1_p113_Oriolo
work_keys_str_mv AT oriolosebastian crossstrikestructurescontrollingmagmatismemplacementinaflatslabsettingprecordilleracentralandesofargentina
AT japasmariasilvia crossstrikestructurescontrollingmagmatismemplacementinaflatslabsettingprecordilleracentralandesofargentina
AT cristalliniernestoosvaldo crossstrikestructurescontrollingmagmatismemplacementinaflatslabsettingprecordilleracentralandesofargentina
_version_ 1768545284729602048

Ejemplares similares