Geochemical Mapping of Iron Quadrangle region by active stream sediments, State of Minas Gerais, Brazil

JOÃO HENRIQUE LARIZZATTI, EDUARDO DUARTE MARQUES, FRANCISCO VALDIR SILVEIRA

Abstract


The geochemical survey of Iron Quadrangle was performed by the Geological Survey of Brazil - CPRM involving geochemical data from the area between 42°30’W and 45°W and 19°30’S and 21°S, totalling 45.000 km2. Active stream sediment was analyzed. Fine fractions (< 80# or 0.175 mm) were pulverized to –150# fraction (~ 0.100 mm), digested by hot acqua regia and analyzed for 53 elements by ICPMS. Maps of raw and manipulated data (element concentrations and multi-elemental scores) were made. Stream sediment (< 80# fraction) is an effective sampling medium for regional geochemical surveys. Geochemical structures, lithological units and mineralization processes were recognized with the sample density of 1 sample per 12 km2. Sample density has a key role in the quality of the geochemical maps produced. Caution must be taken when interpreting the results because of its nature; these data do not necessarily pinpoint specific geochemical anomalies or single ore deposits. The interpretation of stream sediment samples is not straightforward and must take into account secondary processes involved in the evolution of sampling media. These data may be used in mineral exploration to delineate favorable targets for more detailed studies. Mineral deposits often occur in geochemical provinces characterized by elevated concentration of elements of economic interest and pathfinder elements. Ore deposits tend to cluster along specific stratigraphic units and/or structural trends over large areas. These geochemical data can be used in environmental studies, support decision makers in the definition of public policies and in the management of sustainable land use.


Keywords


Geochemical mapping; Stream sediment; Iron Quadrangle; Mineral exploration; Geological mapping.

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DOI: http://dx.doi.org/10.21715/GB2358-2812.2018322268

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