Publication: Tectónica alpina y morfogénesis
en el Sistema Central español:
Modelo de deformación intracontinental distribuida
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Publication Date
1986
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Sociedad Geológica de España
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Abstract
The formation of the Spanish Central System is a adscribed to an intracontinental shear zone whose activity implies rotation of blocks within areas of intense deformation. This model of distributed deformation explains the fragmented shape of the relief and can be referred to the intraplate deformation of Iberia.