La evolución de los minerales de la arcilla en la cuenca de Lorca (Murcia)

Abstract

The clay mineral association of the Lorca basin (Murcia) is built by muscovite, chlorite (clinochlore), montmorillonite, kaolinite and something of paragonite. The application of statistical methods, the factor analysis and the analysis mineralogical: space-temporal distribution, mineral associations, mufua/ relationships and crystalchemical parameters, have allowed to know the possible source areas, the processes of transport and sedimentation-and climatology in each TSU