Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Jesús Aller"'
Publikováno v:
Scopus
RUO: Repositorio Institucional de la Universidad de Oviedo
Universidad de Oviedo (UNIOVI)
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
RUO: Repositorio Institucional de la Universidad de Oviedo
Universidad de Oviedo (UNIOVI)
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
Financial support came from the Spanish Ministerio de Economia y Competitividad (project CGL2015-66997-R).
Publikováno v:
Journal of Structural Geology. 112:69-80
A new mechanism, named “heterogeneous rotation shear”, is defined to explain the development of similar folds. It is based on the heterogeneous distribution of a type of deformation in which a line rotates without length change and another mainta
Publikováno v:
Journal of Structural Geology. 112:131-137
We define a simple two-dimensional deformation called “rotation shear”. It has one line of no finite longitudinal strain with invariant direction and another one that rotates with the deformation. An analysis of this deformation is carried out. R
Publikováno v:
International Journal of Earth Sciences. 107:2727-2740
The paleothermometric evolution of the Ponga unit at the core of the Cantabrian Zone, the arcuate foreland fold and thrust belt of the Variscan orogen in NW Spain, is analyzed using the conodont Color Alteration Index and the Kübler Index of illite.
Publikováno v:
Journal of Structural Geology. 94:213-226
An outcrop on the Cantabrian coast (Burela section) shows a long train of tight meter-scale folds developed in Cambrian siliciclastic rocks. These folds have been shortened in the axial trace direction on the fold profile, developing a cleavage in th
Publikováno v:
Solid Earth, Vol 7, Iss 4, Pp 1003-1022 (2016)
Scopus
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
Scopus
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
The tectonothermal evolution of an area located in the core of the Ibero-Armorican Arc (Variscan belt) has been determined by using the conodont colour alteration index (CAI), Kübler index of illite (KI), the Árkai index of chlorite (AI) and the an
Publikováno v:
BSGF-Earth Sciences Bulletin, Vol 191, p 6 (2020)
WOS:000519538100002
RUO: Repositorio Institucional de la Universidad de Oviedo
Universidad de Oviedo (UNIOVI)
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
WOS:000519538100002
RUO: Repositorio Institucional de la Universidad de Oviedo
Universidad de Oviedo (UNIOVI)
RUO. Repositorio Institucional de la Universidad de Oviedo
instname
A field analysis of kink bands developed in slates from three areas (Grandas, Boal and Luarca areas) of the Westasturian-Leonese Zone (Iberian Variscan belt) is presented. The analysis of the main parameters that characterize the geometry of the stud
Publikováno v:
Computers & Geosciences. 78:123-132
StrainModeler is a program constructed in the Mathematica ™ environment that performs 3D progressive strain calculations for lines and planes undergoing any sequence of homogeneous deformations. The main inputs to the system define the initial line
Autor:
Omar Menéndez, Fernando Bastida, Nilo C. Bobillo-Ares, Francisco J. Fernández, Jesús Aller, Richard John Lisle
Publikováno v:
Earth-Science Reviews. 135:162-183
This review has two main parts. The first of them presents existing ideas and data related to recumbent folds, reviewing aspects such as the physical conditions of the development of these folds, the strain inside the folded layers, the kinematic mec
Autor:
Javier Sanz-López, Jesús Aller, Silvia Blanco-Ferrera, Fernando Bastida, Susana García-López, José A. Marín
Publikováno v:
Geological Magazine. 150:1047-1061
The tectonothermal evolution of a unit in the foreland fold-and-thrust belt of the Iberian massif is established using the conodont colour alteration index (CAI). The unit consists of two parts with different tectonothermal histories – the Esla nap