Zaccarini, FedericaPortella, Yuri de M. [UNESP]Bakker, Ronald J.Angeli, Nelson [UNESP]Garuti, GiorgioThalhammer, Oskar A. R.2014-05-202014-05-202012-04-01Neues Jahrbuch Fur Mineralogie-abhandlungen. Stuttgart: E Schweizerbartsche Verlags, v. 189, n. 2, p. 207-215, 2012.0077-7757http://hdl.handle.net/11449/25194Monazite from chromitites of Cedrolina (Goias State, Brazil) was investigated by electron microprobe and Raman spectroscopy. Monazite has been rarely encountered in chromitites. In Brazil, it was previously reported from chromitites of the Campo Formoso layered intrusion. Comparison between the two occurrences indicates similar morphology and textural characteristics, but remarkable differences in chemical composition. In both cases, monazite occurs as irregular grains (up to 200 mu m) preferentially located in the chlorite-serpentine matrix of the chromitite, more rarely included in chromite. However, the monazite from Cedrolina is characterized by higher Ce/La ratio, and Pr, Nd, Th contents, compared with the monazite from Campo Formoso. The obtained Raman spectra are very similar in the two cases, suggesting that the compositional variation of monazites and the spectral resolution of the Raman do not allow a conclusive chemical analysis with Raman spectra. Textural evidence indicates that, in both occurrences, monazite precipitation did not take place at high temperature, concomitantly with the host chromitite. In the Campo Formoso chromitites, precipitation of monazite has been related with percolation of hydrothermal, aqueous and acid fluids emanating from a granite batholith. on the contrary, the Cedrolina monazite probably formed during one of the metamorphic events that affected the area in which the host chromitite occurs.207-215engmonazitechromititeCedrolinaBrazilRamanelectron microprobemetamorphismPilar de Goias greenstone beltArtigo10.1127/0077-7757/2012/0220WOS:000303482700008Acesso restrito0864918679971906