Artigo Revisado por pares

Delamination in the Betic Range: Deep structure, seismicity, and GPS motion

2013; Geological Society of America; Volume: 41; Issue: 3 Linguagem: Inglês

10.1130/g33733.1

ISSN

1943-2682

Autores

Flor de Lis Mancilla, Daniel Stich, Manuel Berrocoso, Rosa Martín, J. Morales, A. Fernández-Ros, R. Páez, Alejandro Pérez-Peña,

Tópico(s)

Pneumothorax, Barotrauma, Emphysema

Resumo

Research Article| March 01, 2013 Delamination in the Betic Range: Deep structure, seismicity, and GPS motion Flor de Lis Mancilla; Flor de Lis Mancilla 1Instituto Andaluz de Geofísica, Universidad de Granada, 18071-Granada, Spain2Departamento de Física Teórica y del Cosmos, Universidad de Granada, 18071-Granada, Spain Search for other works by this author on: GSW Google Scholar Daniel Stich; Daniel Stich 1Instituto Andaluz de Geofísica, Universidad de Granada, 18071-Granada, Spain2Departamento de Física Teórica y del Cosmos, Universidad de Granada, 18071-Granada, Spain Search for other works by this author on: GSW Google Scholar Manuel Berrocoso; Manuel Berrocoso 3Laboratorio de Astronomía, Geodesia y Cartografía, Departamento de Matemáticas, Universidad de Cádiz, 11510 Puerto Real, Cádiz, Spain Search for other works by this author on: GSW Google Scholar Rosa Martín; Rosa Martín 1Instituto Andaluz de Geofísica, Universidad de Granada, 18071-Granada, Spain Search for other works by this author on: GSW Google Scholar José Morales; José Morales 1Instituto Andaluz de Geofísica, Universidad de Granada, 18071-Granada, Spain2Departamento de Física Teórica y del Cosmos, Universidad de Granada, 18071-Granada, Spain Search for other works by this author on: GSW Google Scholar Alberto Fernandez-Ros; Alberto Fernandez-Ros 3Laboratorio de Astronomía, Geodesia y Cartografía, Departamento de Matemáticas, Universidad de Cádiz, 11510 Puerto Real, Cádiz, Spain Search for other works by this author on: GSW Google Scholar Raúl Páez; Raúl Páez 3Laboratorio de Astronomía, Geodesia y Cartografía, Departamento de Matemáticas, Universidad de Cádiz, 11510 Puerto Real, Cádiz, Spain Search for other works by this author on: GSW Google Scholar Alejandro Pérez-Peña Alejandro Pérez-Peña 3Laboratorio de Astronomía, Geodesia y Cartografía, Departamento de Matemáticas, Universidad de Cádiz, 11510 Puerto Real, Cádiz, Spain Search for other works by this author on: GSW Google Scholar Author and Article Information Flor de Lis Mancilla 1Instituto Andaluz de Geofísica, Universidad de Granada, 18071-Granada, Spain2Departamento de Física Teórica y del Cosmos, Universidad de Granada, 18071-Granada, Spain Daniel Stich 1Instituto Andaluz de Geofísica, Universidad de Granada, 18071-Granada, Spain2Departamento de Física Teórica y del Cosmos, Universidad de Granada, 18071-Granada, Spain Manuel Berrocoso 3Laboratorio de Astronomía, Geodesia y Cartografía, Departamento de Matemáticas, Universidad de Cádiz, 11510 Puerto Real, Cádiz, Spain Rosa Martín 1Instituto Andaluz de Geofísica, Universidad de Granada, 18071-Granada, Spain José Morales 1Instituto Andaluz de Geofísica, Universidad de Granada, 18071-Granada, Spain2Departamento de Física Teórica y del Cosmos, Universidad de Granada, 18071-Granada, Spain Alberto Fernandez-Ros 3Laboratorio de Astronomía, Geodesia y Cartografía, Departamento de Matemáticas, Universidad de Cádiz, 11510 Puerto Real, Cádiz, Spain Raúl Páez 3Laboratorio de Astronomía, Geodesia y Cartografía, Departamento de Matemáticas, Universidad de Cádiz, 11510 Puerto Real, Cádiz, Spain Alejandro Pérez-Peña 3Laboratorio de Astronomía, Geodesia y Cartografía, Departamento de Matemáticas, Universidad de Cádiz, 11510 Puerto Real, Cádiz, Spain Publisher: Geological Society of America Received: 11 Jun 2012 Revision Received: 27 Aug 2012 Accepted: 30 Sep 2012 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2013 Geological Society of America Geology (2013) 41 (3): 307–310. https://doi.org/10.1130/G33733.1 Article history Received: 11 Jun 2012 Revision Received: 27 Aug 2012 Accepted: 30 Sep 2012 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Flor de Lis Mancilla, Daniel Stich, Manuel Berrocoso, Rosa Martín, José Morales, Alberto Fernandez-Ros, Raúl Páez, Alejandro Pérez-Peña; Delamination in the Betic Range: Deep structure, seismicity, and GPS motion. Geology 2013;; 41 (3): 307–310. doi: https://doi.org/10.1130/G33733.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Subduction comes to an end when all oceanic lithosphere is consumed and continental or transitional crust, with positive buoyancy, becomes involved. During continental collision, the final stage of subduction may be characterized by slab breakoff, limited continental subduction, and delamination below the fold-and-thrust belt. We report receiver function images, constructed from a dense array of seismic broadband stations, that reveal the underthrusting of Iberia beneath the Alboran plate. The underthrusted crust is delaminating beneath part of the Betic mountain range, still connected to the foreland lithosphere on one side, and interrupted discontinuously along the other side. Intermediate deep earthquakes associated with the delamination process do not respond to downdip stresses like subduction earthquakes. The GPS velocity field and source mechanisms for shallow earthquakes demonstrate ongoing active shortening on top of the hinge of delamination, and localized perpendicular extension on top of the edge of delamination, introducing independent motion of the overriding crustal block. Delamination beneath the Betic Range drives seismicity by inducing fundamental changes in deformation patterns within the collision orogen. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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