Nuevos datos para la estimación de los valores de levantamiento desde el Tortoniense Superior a la actualidad en la parte centro-occidental de la Sierra de Carrascoy (provincia de Murcia)
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Abstract
The existence of sediments of the Late Tortonian near the top, and in the slopes, of Sierra de Carrascoy, deposited above a former erosionaI surface excavated in the basement, permits precise estimation of the vertical displacements occurred in this are a in the last 5 m.a. The value of 0,2 mm/y has been exceeded in several moments of this interval of time
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