The Torres Cartas Fault Zone is a large low-angle extensional structure, strongly thinning the Nevado-Filabride and Alpujarride nappes. These nappe complexes form the basement of the Alboran sea southwest Sierra Alhamilla. The fault zone, being already probably active in Burdigalian times, was folded during the Upper MioceneLa zona de fallas de Torres Cartas es una estructura grande y de bajo ángulo entre Nevado-Filábride y los mantos de Alpujárrides. Estos complejos mantos forman el subsuelo del mar de Alborán, al suroeste de la Sierra Alhamilla. La zona de fallas, probablemente activa desde tiempos Burdigalianos, fue plegada durante el Mioceno Superior
The Campo de Dalias is an emerged zone located at the northern boundary of Alboran Sea. The Neogene-...
The Calatayud-Daroca Basin is located in the Iberian Range. The SW margin of this Basin is the Jiloc...
13 páginas, 7 figuras.[EN] The southern border of the Sorbas-Tabernas neogene basin is formed by imp...
The Alpujarride complex located to the South of the Sierra Nevada and extending between Motril and A...
In the Alboran Domain, the Alpujarride/Nevado-Filabride major boundary is a brittleductile and britt...
During the Miocene rift in gof the Alboran Domain, various extensional systems developed. North of S...
The southern edge of the Granada basin is delimited by faults trending in an E-W to N 100-120 E dire...
La Falla del Norte de Tabarca, de traza E-O, es el límite norte de la cresta anticlinal de Tabarca, ...
The Gulf of California Extensional Province in northeastern Baja California contains a major structu...
Low angle normal faults (LANF) related with extensional detachments are mapped in the Western Betics...
Pliocene to Holocene alluvial and colluvial deposits in the Granada Depression and surrounding areas...
Reunión Ibérica sobre Fallas Activas y Paleosismología (3ª. 2018. Alicante). - Texto en español con ...
The position and kinematics of shear zones, which developed under different P-T conditions, lead to ...
55 pages, 13 figuresThe Alboran Basin is a Neogene-Quaternary extensional basin located within the B...
In the Central Betics, the Alpujarride Complex is made up of units which result from the dismemberin...
The Campo de Dalias is an emerged zone located at the northern boundary of Alboran Sea. The Neogene-...
The Calatayud-Daroca Basin is located in the Iberian Range. The SW margin of this Basin is the Jiloc...
13 páginas, 7 figuras.[EN] The southern border of the Sorbas-Tabernas neogene basin is formed by imp...
The Alpujarride complex located to the South of the Sierra Nevada and extending between Motril and A...
In the Alboran Domain, the Alpujarride/Nevado-Filabride major boundary is a brittleductile and britt...
During the Miocene rift in gof the Alboran Domain, various extensional systems developed. North of S...
The southern edge of the Granada basin is delimited by faults trending in an E-W to N 100-120 E dire...
La Falla del Norte de Tabarca, de traza E-O, es el límite norte de la cresta anticlinal de Tabarca, ...
The Gulf of California Extensional Province in northeastern Baja California contains a major structu...
Low angle normal faults (LANF) related with extensional detachments are mapped in the Western Betics...
Pliocene to Holocene alluvial and colluvial deposits in the Granada Depression and surrounding areas...
Reunión Ibérica sobre Fallas Activas y Paleosismología (3ª. 2018. Alicante). - Texto en español con ...
The position and kinematics of shear zones, which developed under different P-T conditions, lead to ...
55 pages, 13 figuresThe Alboran Basin is a Neogene-Quaternary extensional basin located within the B...
In the Central Betics, the Alpujarride Complex is made up of units which result from the dismemberin...
The Campo de Dalias is an emerged zone located at the northern boundary of Alboran Sea. The Neogene-...
The Calatayud-Daroca Basin is located in the Iberian Range. The SW margin of this Basin is the Jiloc...
13 páginas, 7 figuras.[EN] The southern border of the Sorbas-Tabernas neogene basin is formed by imp...
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