Airborne gamma-ray spectrometric and magnetic signatures of fazenda nova region, East portion of arenópolis magmatic arc, Goiás

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Abstract

Airborne geophysical data are an important tool for the interpretation of geological features. The variations observed in airborne magnetic and gamma-ray spectrometric data are typically used to differentiate geological units and delimit structures. In this context, this study aims to use gamma-ray spectrometric and magnetic airborne data to support the geological mapping in the Fazenda Nova region, located in the east portion of the Arenópolis Magmatic Arc. The processing of the gamma-ray spectrometric data consisted of generating K, U, Th, total count, gamma-ray spectrometric ratios and ternary images. The anomalous magnetic field processing and enhancing generated the magnetic maps, which provided information about the structural framework of the area, while the gamma-ray profiles and images allowed the delineation of the geologic-geophysical domains. Fifteen domains were individualized, interpreted especially from ternary images, which displayed a good relation with the granite bodies mapped and indicated different rocks associated with the Goiás Alkaline Province, contributing to improving the geological knowledge of the area.

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APA

Ramos, L. N. R. A., Pires, A. C. B., & Toledo, C. L. B. (2014). Airborne gamma-ray spectrometric and magnetic signatures of fazenda nova region, East portion of arenópolis magmatic arc, Goiás. Revista Brasileira de Geofisica, 32(1), 123–140. https://doi.org/10.22564/rbgf.v32i1.401

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