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The Espinhaço Range is an expressive geomorphological landmark that covers more than 1200km in a north-south general trend through the Brazilian states of Minas Gerais and Bahia, being called Espinhaço Meridional Range (EMR), southwards of the 17°00' S parallel (Knauer, 2007). The evolu onary history of the São Francisco Craton (SFC) is intrinsically related to the deposi on of the rocks that sustain the EMR (Espinhaço Supergroup). The individualiza on of the cratonic area took place from the Paleo to Neoproterozoic, with the establishment of STRATIGRAPHIC AND STRUCTURAL RELATIONSHIPS THROUGH GEOLOGICAL AND

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STRATIGRAPHIC AND STRUCTURAL RELATIONSHIPS THROUGH GEOLOGICAL AND GAMMAESPECTROMETRY ANALYSIS IN THE INTERFACE BETWEEN THE SÃO FRANCISCO CRATON AND THE ARAÇUAÍ OROGEN (SANTA RITA ANTICLINE, MINAS GERAIS, BRAZIL)