In Montalban Anticline North Zone (Paleozoic basement of the lberian Chain) a magmatism with calc-alkaline affinity, characterized by numerous Stephanian-Permian hypovolcanic intrusions, wich intruded in both carboniferous and devonian sediments, is well represented.
Sorne examples about the intrusions emplacement forms as well as a preliminary analysis of the country rock structure are shown.
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