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Recolector de Ciencia Abierta, RECOLECTA
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Distensión-comprensión en la cuenca de Campo Arañuelo. Implicación cortical

descriptionPublicationkeyboard_double_arrow_right Article 01 Jan 1990 Spain Spanish Publisher:Sociedad Geológica de España
Authors: Martín Escorza, Carlos;

handle: 10261/270341 , 10272/18160

Distensión-comprensión en la cuenca de Campo Arañuelo. Implicación cortical

Abstract

Pre-Arcosic detritic sediments (Paleocene-Eocene?) have been affected by normal faults; this distension phase, named Extremeña Phase, is related with Other similar regional observations. During Lower-Upper Miocene a new compressive phase cause thrusting with granite and metamorphic rocks of Gredos ånd Montes of Toledo overthrusting to Pre-Arcosic and Arcosic sediments. This phase is including at the Guadarama, and/or Neocastellana, Phases detected in eastern Central System massiff and other Meseta basins respectivaly.

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Spain
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Keywords

Central Iberian Meseta, Thrust faults, Alpine tectonics, Campo Arañuelo Basin, Normal faults

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popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
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influence
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impulse
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