Modelización de la corteza terrestre en la zona de confluencia de las cordilleras Ibérica y Béticas en base a datos gravimétricos
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Abstract
The results of a gravimetric reseach carried out in the SE of the Iberian Peninsula (areas of Albacete , Valencia and Murcia) allow us to obtain a pattern of the earth's modelling crust, in which the existence of a cortical slimming separating the iberica and Betica chain is observed. This is probably related to arifting process of the SW branch of the triple point of the Valencia basin
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