Génesis y evolución de la fosa de la Cerdanya (Pirineos Orientales)
Roca, E.; Santanach, P.;
Génesis y evolución de la fosa de la Cerdanya (Pirineos Orientales)
La fosa de Cerdanya está situada al final SO de la falla de la Tet, en su bloque NO. Su formación, durante el Mioceno Superior, estuvo condicionada al desplazamiento dextral de esa falla, y al desplazamiento normal E-O de una falla inclinada que absorbió el movimiento de la anterior.
The Cerdanya basin is located at the SW end of the Tet fault, in its NW block. Its formation, during the Upper Miocene, was conditioned by dextral slip of this fault anf the normal slip of E-W trending faults that absorbed the movement of the former
Spain
- University of Huelva Spain
Slip, Basin, Cerdanya, Fault
Slip, Basin, Cerdanya, Fault
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These citations are derived from selected sources.
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
Citations provided by BIP!popularityPopularity provided by BIP!
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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