Ramón Vegas Martínez, L. M. Barranco, Juan Tomás Vázquez
The fracture pattern in Southeastern Spain can be exp/ained in terms of block tectonics.
A detailed analysis of satel/ite images leads to define the main fracture zones and domains as wel/ as the interna/ crusta/ blocks. The kynematic model derived from this analysis can accoun( for the seismic pattern, the neotectonics and the geodynamics of the complex Africa-Eurasia plate boundary.
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