A Formação Água Clara na Região de Araçaíba - SP: registro U-Pb de uma bacia mesoproterozóica

Abstract

The main objective of this work is to present U-Pb isotopic data obtained from zircons of metabasic rocks and subordinate acid and associated rocks of the Agua Clara Formation in the Aracaiba region - Sao Paulo. The Agua Clara Formation is predominantly constituted by a sequence of carbonate rocks (pure to impure marbles), calc-silicate rocks, calc schists, mica schists, amphibole schists, quartzites, garnet-chlorite-biotite schists, metacherts, basic and intermediate metatuffs, metabasites, amphibolites and cornubianites. The metabasic bodies are usually a few km long with widths of hundreds of m. They are greenish gray, fine- to medium-grained, and usually present nematoblastic texture. More isotropic terms also occur, showing granoblastic texture. They are composed of pyroxenes (diopside or augite), amphiboles (actinolite and hornblende), and plagioclases (andesine/oligoclase). The most common accessories are apatite, magnetite, epidote, titanite, and rare zircon. In thin section, preserved ophitic and subophitic textures are observed, indicating a probable igneous origin. The geochemical data suggest compositions similar to enriched midoceanic ridge basalts (E-MORB) tending to oceanic island basalts (OIB). The subalkaline, tholeiitic characteristics, similar to E-MOR basalts tending to OI basalts, suggest distension or back-arc environments as the geotectonic settings for the basic magmatism. The geochronologic and geochemical characteristics and structural patterns described for the Agua Clara Formation metabasic lithotypes (probably sills and/or dikes) suggest that periodic volcanism with associated sedimentation occurred during the Mesoproterozoic at about 1500 Ma. This event represents an important marker in the volcano-sedimentary evolution of the Apiai Domain. The Neoproterozoic values obtained refer to zircon recrystallization, to neoformation processes which affected the metabasics and amphibolites, to the emplacement of granitic and acid volcanic rocks, and to regional cooling of the Agua Clara Formation.