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- W1799128825 abstract "The high grade terrains of the N-S trending polycyclic belt known in Northeastern Bahia have been investigated along the Curaca Valley region, as important copper mineralizations (180 millions tons of ore with 1,0% Cu, mostly in the Caraiba district) were discovered. The Curaca Valley region is essentially formed by granodioritic to tonalitic gneisses (older basement?), Archean metasediments (quartz-feldspathic gneisses, leptynites, cordierite-sillimanite-garnet-biotite gneisses, quartzites, magnetite quartzites, calc-silicate rocks), and associated mafic-ultramafic intrusions. This lithologic assemblage was affected by rnetamorphism of granulite facies and tight folding apparently related to the Jequie event, and was reworked later during the Transamazonian event (retrometamorphic transformations, migmatization, granitization, deformation). The mafic-ultramafic intrusions (hyperstenite-norite-gabbro-anorthosite) are interpreted as being derived from differentiated tholeiitic magma and hostwell known mineralizations (magnetite-chalcopyrite-bornite-ilmenite, sorne pyrrhotite and pyrite, scarce pentlandite, violarite, millerite, tetrahedrite, hematite)." @default.
- W1799128825 created "2016-06-24" @default.
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- W1799128825 date "1982-01-01" @default.
- W1799128825 modified "2023-09-23" @default.
- W1799128825 title "GEOLOGY AND COPPER MINERALIZATION OF CURAÇÁ RIVER VALLEY, BAHIA" @default.
- W1799128825 doi "https://doi.org/10.5327/rbg.v12i1-2-3.290" @default.
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