Carlos Sanz de Galdeano Equiza, Ángel Carlos López Garrido, Francisco Juan García Tortosa
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
© 2001-2024 Fundación Dialnet · Todos los derechos reservados