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Transtensión y transpresión del Jurásico Medio-Superior al Cretácico Inferior durante la construcción del arco magmático en Chile central: evidencia a partir de enjambres de diques máficos
(Servicio Nacional de Geología y Minería (SERNAGEOMIN), 2011)
Transtension controlling volcanic morphology: Insights from oblique-to-the arc tectonic domains
(2014)
Long
and
short-‐term
tectonic
activity
plays
an
essential
role
in
the
segregation,
transport
and
emplacement
of
fluids
and
magmas
within
the
continental
crust.
Magma
ascent
and
emplacement
mechanisms
within
volcanic
arc ...
Detrital zircon fission-track thermochronology and magnetic fabric of the Amagá Formation (Colombia): Intracontinental deformation and exhumation events in the northwestern Andes
(ELSEVIER SCIENCE BV, 2017-07-01)
New detrital zircon-fission track (ZFT) and magnetic fabric data are presented to constrain the time of deposition, provenance and deformation of the of Lower and Upper members of the Amagá Formation in the Amagá Basin. ...
Caracterización estructural de la cordillera Chongón Colonche entre el cantón Guayaquil y Daule en el sector de Pascuales, Provincia del Guayas
(Facultad de Ciencias Naturales. Universidad de Guayaquil, 2019-09)
La presente investigación tuvo como objetivo determinar las características geológicas y estructurales de los afloramientos de la Cordillera Chongón Colonche en el sector Pascuales, ubicado entre los cantones Guayaquil y ...
Transpressional motions along the Cordillera Occidental - coastal belt boundary since the Late Cretaceous (southern Peru, 16°S)
(IRD ÉditionsFRA, 2002)
The study area is located in southern Peru NW of the city of Arequipa (16° S) at the boundary between the Cordillera Occidental and coastal belt. Previous studies sustain that exists in the area a large overthrust, named ...
Transtension driving volcano-edifice anatomy: Insights from Andean transverse-to-the-orogen tectonic domains.
(2016)
Dykes and minor eruptive vents are not randomly distributed within tectonically controlled volcanic arcs, which is reflected in the resulting morphology of stratovolcanoes. As a first-order approach, regional stress field ...
Middle-Late Jurassic to Early Cretaceous transtension and transpression during arc building in Central Chile: evidence from mafic dike swarms.
(2011)
The Middle-Late Jurassic mafic dike swarms of central Chile between 33 degrees and 33 degrees 45'S register the tectonic activity of the contemporaneous arc represented by the Coastal batholith. These dike swarms evidence ...