Geophysical Prospecting Over a Meta-Ultramafic Sequence with Indicators of Gold Mineralization in Rio Grande do Sul Stat
- PDF / 7,482,462 Bytes
- 17 Pages / 547.087 x 737.008 pts Page_size
- 47 Downloads / 231 Views
Pure and Applied Geophysics
Geophysical Prospecting Over a Meta-Ultramafic Sequence with Indicators of Gold Mineralization in Rio Grande do Sul State, Southernmost Brazil BRUNO DANIEL LENHARE1 Abstract—This work investigates the occurrence of gold on meta-ultramafic rocks at Funcho Farm, Sa˜o Sepe´, Rio Grande do Sul state, southernmost Brazil. The presence of base metals in meta-ultramafic rocks whose origin is related to volcanic massive sulfide (VMS) deposits has only rarely been explored in the scientific literature. The gold was identified in geochemical prospecting of current sediments in previous works, and suggested that the host rock of the mineralization is the serpentinite of Funcho Farm. The methodology used to achieve the study objectives included geological field surveys, surveys of structural measurements and acquisition of geophysical data utilizing electrical resistivity (DC) and induced polarization (IP) methods, using electrical tomography, with the execution of dipole–dipole arrays. In this study, nine electrical tomography lines, each 400 m, were acquired. The data were processed in 2D electrical inversion and then interpolated for 3D visualization. The information acquired for interpretations during field studies revealed that the probable mineralization is hosted in structures such as fractures and hinges and is also associated with milky quartz veins. The data analysis allowed the 3D delimitation of possible deep sulfide mineralizations from hydrothermal fluids, probably from the intrusion of the Sa˜o Sepe´ granite. The results presented in this work are very useful, because they can serve as an appropriate analogy of geological reality associated with a reliable deposit architecture, helping to outline a strategy for a future drilling campaign directed to the targets found. Keywords: Mineral research, resistivity, chargeability, electrical tomography, gold, meta-ultramafic.
1 Universidade Estadual Paulista, UNESP/Rio Claro Campus, Avenida 24-A, 1515-Bela Vista, PO Box 178. 13506-900, Rio Claro, SP, Brazil. E-mail: [email protected] 2 Department of Geology, DGA, Universidade Estadual Paulista, UNESP/Rio Claro Campus, Avenida 24-A, 1515-Bela Vista, PO Box 178, Rio Claro, SP 13506-900, Brazil. E-mail: [email protected]
and CE´SAR AUGUSTO MOREIRA2 1. Introduction Ancient meta-ultramafic rocks of the ArcheanProterozoic whose origin may relate to ophiolites commonly host chromite mineralizations, but mineralizations of final phases of magmatic crystallization, such as sulfides and gold, are rare (Berger 2013; Groves et al. 1998). Rocks of this nature have been subjected to several later tectonic cycles, and metamorphic records of these lithotypes are common as serpentinites in greenstone belts (Powell et al. 1991). The metamorphic and deformation events imply deformations and generation of lower-pressure zones, and eventual spaces for accommodation of hydrothermal fluids from other rocks, in the context of regional deformation events. Although they are neglected rocks for sulfide base m
Data Loading...
