Magnetic susceptibility of Variscan granite-types of the Spanish Central System and the redox state of magma


  • C. VILLASECA Dpto. Petrología y Geoquímica, Facultad C.C. Geológicas, Universidad Complutense Madrid. Instituto de Geociencias (IGEO) (Universidad Complutense de Madrid, CSiC) Madrid, Spain.
  • V.C. RUIZ-MARTÍNEZ Dpto. Física de la tierra AAI, Facultad CC Físicas, universidad Complutense Madrid, Spain.
  • C. PÉREZ-SOBA Dpto. Petrología y Geoquímica, Facultad C.C. Geológicas, Universidad Complutense, Madrid.


Magnetic susceptibility, Granite type, Biotite chemistry, Oxygen fugacity.


Magnetic susceptibility (MS) has been measured in Variscan granites from central Spain. They yield values in the order of 15 to 180μSI units for S- and I-type granites, indicating that both types belong to the ilmenite series. Only samples from magnetite-bearing leucogranites from the I-type La Pedriza massif show high MS values, in the order of 500-1400μSI, reflecting the presence of this ferromagnetic mineral. Mineral chemistry of magmatic Fe-rich minerals (mainly biotite) suggests similar oxidation values for both granite types. MS values change in highly fractionated granites accordingly either with the presence of rare new Fe-oxide phases (some I-type leucogranites) or with the marked modal amount decrease of Fe-rich minerals (I- and S-type leucogranites). The redox state in highly fractionated granite melts is mostly controlled by magmatic processes that modify redox conditions inherited from the source region. Thus, the occurrence of magnetite or ilmenite in granites is primarily controlled by the oxidation state of the source material but also by the differentiation degree of the granite melt. The presence of magnetite in some Variscan I-type leucogranites might be a consequence of crystal fractionation processes in a more limited mafic mineral assemblage than in S-type granite melts.






Granites and Related Rocks. A tribute to Guillermo Corretgé