Historia geológica de la cuenca de Lorca (Murcia): influencia de la tectónica en la sedimentación
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Abstract
Neogene sedimentation in the Lorca basin has been related to tectonics specially to Basin's Central Fault, whic has alternately like inverse and normal according to compressive ord is tensible phases; likewise the depocentre has been displaced successively to one side and the other of the fore-mentioned accident.
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