Arc-parallel vs back-arc extension in the Western Gibraltar arcIs the Gibraltar ferearc still active?
- Balanyá Roure, Juan Carlos
- Crespo Blanc, Ana
- Díaz Azpiroz, Manuel
- Expósito Ramos, Inmaculada
- Torcal Medina, Federico
- Pérez Peña, José Vicente
- Booth Rea, Guillermo
ISSN: 1695-6133
Año de publicación: 2012
Volumen: 10
Número: 3
Páginas: 249-264
Tipo: Artículo
Otras publicaciones en: Geologica acta: an international earth science journal
Resumen
Extremely tight arcs, framed within the Eurasia-Africa convergence region, developed during the Neogene on both sides of the western Mediterranean. A complex interplate deformation zone has been invoked to explain their structural trend-line patterns, the shortening directions and the development of back-arc basins. Updated structural and kinematic maps, combined with earthquake data covering the complete hinge zone of the western Gibraltar arc help us to explore the mode of strain partitioning from 25My ago to present. During the Miocene, the strain partitioning pattern showed arc-perpendicular shortening in the active orogenic wedge �assessed from the radial pattern of tectonic transport directions� accompained by subhorizontal stretching. Structures accommodating stretching fall into two categories on the basis of their space distribution and their relationships with the structural trend-line pattern: i) arc-parallel stretching structures in the external wedge (mainly normal faults and conjugate strike-slip faults); and ii) extensional faults developed in the hinterland zone in which transport directions are centripetal towards the Alborán back-arc basin. Pliocene to Recent deformational structures together with focal solutions from crustal earthquakes (n=167; 1.5