Caracterização química de cromitas nos maciços de cromínia e mairipotaba, goiás, Brasil
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Data
2010-03-01
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Metaultramafic bodies tectonically emplaced within the metasedimentary sequence of the Araxá Group are associated with an ophiolitic melange in southeast Goiás. In the region of Crominia - Mairipotaba, they occur as lenticular bodies aligned E-W. Cumulate textures and geochemical data indicate that the parent rocks had harzburgitic to dunitic compositions. Relicts of primary crystals of olivine and orthopyroxene are suggestive of amphibolite facies metamorphic re-equilibration fabrics, even though the paragenesis and mineral associations of these metaultramafic rocks are typical of greenschist facies (T < 550°C and P = 5.5 kbar). The chromitites exhibit massive to breccioid structure and pull-apart texture, with chromite crystals around 0.5 mm in size. Chromite concentrations in the chromitite levels reach 70 to 85% by volume of the rock. The crystals are dispersed in the matrix, which is composed essentially of serpentine, and subordinately of chlorite and talc. The textures and geochemical data (Cr 2O 3 x TiO 2 and Mg x Cr ratios present in the chromitite) are similar to those observed in ophiolitic complexes. Hence, they correspond to allochthonous bodies (Alpine type) associated with an ophiolitic mélange.
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Araxá group , Brasilia belt , Chromite , Mineral chemistry , Ophiolitic melange , chemical composition , chromite , chromitite , concentration (composition) , geochemistry , greenschist facies , melange , olivine , ophiolite , orthopyroxene , paragenesis , parent body , source rock , Brasilia Belt , Brazil , Goias
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Português
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Geologia USP - Serie Cientifica, v. 10, n. 1, p. 87-99, 2010.