Changes in dip and frictional properties of the basal detachment controlling orogenic wedge propagation and frontal collapse: The external central Betics case

Author:

Jimenez-Bonilla A.1ORCID,Torvela T.2ORCID,Balanyá J. C.1,Expósito I.1ORCID,Díaz-Azpiroz M.1ORCID

Affiliation:

1. Departamento de Sistemas Físicos, Químicos y Naturales; Universidad Pablo de Olavide; Sevilla Spain

2. School of Earth and Environment; University of Leeds; Leeds UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference103 articles.

1. Analogue sandbox models of thrust wedges with variable basal frictions;Argawal;Gondwana Res.,2002

2. Fallas y despegues extensionales en el Subbético Central: Implicaciones en la evolución Neógena de Las Zona Externa de la Cordillera Bética;Azañón;Geogaceta,2012

3. Relief and drainage evolution during the exhumation of the Sierra Nevada (SE Spain): Is denudation keeping pace with uplift?;Azañón;Tectonophysics,2015

4. The effect of spatial distribution of Hormuz salt on deformation style in the Zagros fold and thrust belt: An analogue modelling approach;Bahroudi;J. Geol. Soc. London,2003

5. Effect of ductile and frictional décollements on style of extension;Bahroudi;J. Struct. Geol.,2003

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