A multidisciplinary scientific test (morphotectonic, geophysical, seismic) is proposed for the determination of active seismogenetic sources in the Eastern Castilian Betic Foreland (ABCO). The physical environment of the ABCO would correspond to one of a certain tectonic complexity, characterized by a mode of fragile distributed and hierarchical resolution -on the lithospheric surface- of tectonic efforts in favor of either morphotectonic domains that define elevations and/or oriented depressions, and/or in favor of morphotectonic domains defining lateral escapes. The predominance of one or another possibility of defining "morphotectonic domain" would be, here conditioned to the spatial arrangement of these with respect to the structure of the Arch of Cazorla-Alcaraz-Hellín (ACAH). The current seismogenetic sources would be conditioned by this mode of fragile distributed and hierarchical resolution -on the lithospheric surface- of tectonic efforts.
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