Estudio geoquímico de rocas ígneas del norte de la provincia de Cáceres

Abstract

In this paper is defined the inverse zoned character of the lálama batholith and also its contamination by assimilation from the wall rocks. The dykes with associated mineralisation of scheelite are classified as tholeiitic basalts or hyperaluminous basalts. The relations of this mineralisation with these igneous rocks are discussed.