Termobarometría en los gneises de la unidad extensional de Bentomiz, Complejo Alpujárride (Béticas centrales)
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Abstract
In the gneis of the Bentomiz extensional unit (Sierra Tejeda area), the alpine metamorphic evolution was studied. These rocks show high pressure-high temperature (HP/HT) assemblages. An extensional deformation before Neogene has been recognized in the Aipujarride Complex.












