ÓXIDOS DE FE E TI DO DEPÓSITO DE COBRE DE SURUBIM, VALE DO CURAÇÁ, BA

ROSA MARIA DA SILVEIRA BELLO, JOSE VICENTE VALARELLI, JOHILDO S. FIGUEIREDO BARBOSA, RAINER SCHULTZ GUTTLER
1988 Revista Brasileira de Geociências  
Fe AND Ti OXIDES FROM THE SURUBIM COPPER DEPOSIT, CURA<;:A VALLEY, BAHIA. The Surubim copper deposit belongs to the Curaca River Valley Copper Province, Bahia, characterized by high-grade precambrian terranes. The mineralization is present as disseminated copper and iron sulfides in granulitic bodies with mafic-ultramafic compositions, enclosed in gneisses of several kinds. Lenses of calc-silicate rocks and iron-formations, besides garnet-rich or graphitic horizons, occur associated with these
more » ... ociated with these rocks. The iron-titanium oxides, frequent in mineralized and country rocks, are associated with sulfides and certain silicates. Mineralogical, textural and paragenetic aspects of these minerals, and the application of geothermometry/oxygen barometry methos in coexisting magnetite-ilmenite reflect the complexity of the post-granulitic subsolidus cooling history. The data suggest that these reequilibrations ceased at quite low temperatures, and reached oxygen fugacities close to the HM buffer curve. The T and.10 2 conditions in the peak of the granulitic metamorphism were obtained from geothermobarometric methods, with the original oxide composition estimated. Depending on the method used to recalc ulate the original composition of the i1 menites, the followi ng T and 10 2 ranges were determined: T = 617 to 780 0 Cnog / 0 2 = -17,68 to -13,37 and T = 675 to 780°Cnog / 0 = -15,24 to -13 ,37. In a T x log/02 diagram these values are located close to or slightly abo ve the QMFbuffer curve. These results define the-peak of the granulitic metamorphism, with average temperatures similar to those obtained by other geothermometric methods.
doi:10.25249/0375-7536.1988182149161 fatcat:s2zqwii7enanbp53yn3jo4br5m