The Goiás Massif: Implications for a pre-Columbia 2.2–2.0 Ga continent-wide amalgamation cycle in central Brazil

Cordeiro, Pedro; Oliveira, Claudinei Gouveia de

doi:10.1016/j.precamres.2017.06.021

Cited by 35 publications

(1 citation statement)

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“…The Crixás-Goiás Domain (CGD) [30], formerly the Archean-Paleoproterozoic Terrain of Goiás [31,32], is located in the central-west portion of Goiás, and is part of the Tocantins Province. The province represents a large Brasiliano/Pan-African orogen of the South American Platform formed by a collision between the Amazonian, Paranapanema, and São Francisco/Congo cratons during the Brasiliano Orogeny, which led to the amalgamation of the West Gondwana (Figure 1).…”

Section: Area Geology 21 Crixás-goiás Domainmentioning

confidence: 99%

Electrical Prospecting of Gold Mineralization in Exhalites of the Digo-Digo VMS Occurrence, Central Brazil

do Amaral,

Borges,

Toledo

et al. 2023

Minerals

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The greenstone belts of the Crixás-Goiás Domain are economically important due to significant epigenetic gold deposits and the potential for under-researched syngenetic deposits. The gold occurrences associated with the volcanogenic massive sulfide (VMS) deposits in the region are documented only in the volcanoclastic rocks of the Digo-Digo Formation, Serra de Santa Rita greenstone belt. The objective of this work is to discuss the efficiency of the induced polarization methods in the time and frequency domains for differentiating and identifying potentially mineralized zones in the exhalites associated with the VMS-type gold of the Digo-Digo Formation. Data were acquired using a multielectrode resistivity meter with the dipole–dipole array and 10 m spacing between electrodes, as well as different current injection times (250, 1000, and 2000 ms). After the electrical data processing and inversion, the sections were integrated into ternary red-green-blue and cyan-magenta-yellow models to highlight areas of high chargeability, low resistivity, and high metal factor (frequency domain) and, thus, map the higher potential zones to host polarizable metallic minerals. The geological–geophysical model elaborated from the correlation of electrical and surface geological data allowed us to identify four anomalous areas related to potential mineralized zones. The geological data confirm that two targets are associated with the geological contacts between metamafic and intermediate metavolcanic units and the exhalative horizon. One of the targets coincides with a sulfide-rich exhalative horizon (VMS), while the last target occurs in the occurrence area of metaultramafic rocks, where gold mineralization occurrences have not been previously described, being a promising target for future investigations.

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Section: Area Geology 21 Crixás-goiás Domainmentioning

confidence: 99%