A space to discuss aspects of the Caribbean geology, ore potential of the ophiolite belts, etc.
Monday, April 27, 2026
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This comprehensive technical analysis of the geology and ore potential of Guyana explores the structural evolution of the Guiana Shield and the Amazonian Craton to identify high-value mineral targets. We examine the metallogenic epochs of the Barama-Mazaruni Greenstone Belt, focusing on orogenic gold deposits, lithium exploration in LCT pegmatites, and the transformative 2026 Mineral Inventory mapping project currently underway in the Stabroek block and the interior. The northern region is primarily defined by Paleoproterozoic Orosirian greenstone belts intruded by syn-to-late tectonic granitoids during the Trans-Amazonian Orogeny, a process that facilitated significant mineralization at sites like the 9 Mile Deposit and the Karouni gold deposit (Bassoo & Murphy, 2018; Tedeschi & Hagemann, 2018; Wikipedia, 2025). Advanced exploration data from the Guyana Geology and Mines Commission (GGMC) reveals untapped potential for magmatic Ni-Cu-PGE deposits and critical minerals including tantalum, niobium, and rare earth elements (Lowe, 2013; International Trade Administration, 2026).
While the Liza oilfield discovery has triggered a historic economic boom, the government is utilizing oil revenues to fund a national-scale aerial mineral mapping project intended to diversify the economy before the global energy transition matures (Bloomberg Originals, 2024; Guyana Geology and Mines Commission, 2025). Geochemical studies further highlight the secondary enrichment of REEs and vanadium in lateritic duricrusts and the significant industrial reserves of kyanite in the Supenaam Basin (Ansart et al., 2022; Vieira, 2014). This video provides structural geologists and ore prospectors with a deep dive into the geochemical discrimination of IOCG versus orogenic systems and the long-term mineral endowment of this emerging mining powerhouse (James et al., 2025; Lowe, 2013).
The bridge between Academy and Industry!
P. Geo. Ricardo A Valls, M. Sc. and Geo Gadfly
Valls Geoconsultant
ORCID ID- https://orcid.org/0000-0002-5421-0914
Scopus Author ID: 7003369619/35335510700
ResearcherID: S-6604-2018
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#VallsGeoconsultant #GuyanaGeology #MineralExploration #GuianaShield
Some references:
Ansart, C., Quantin, C., Calmels, D., Allard, T., Roig, J. Y., Coueffe, R., Heller, B., Pinna-Jamme, R., Nouet, J., Reguer, S., Vantelon, D., & Gautheron, C. (2022). (U-Th)/He geochronology constraints on lateritic duricrust formation on the Guiana Shield. Frontiers in Earth Science, 10, Article 888993.
Bassoo, R., & Murphy, J. B. (2018). The 9 Mile Deposit of the Barama-Mazaruni Greenstone Belt of the Guiana Shield: Geochemistry, geochronology and regional significance. Brazilian Journal of Geology, 48(4), 671–683.
James, T., Perrouty, S., & Kontak, D. (2025). Geochemical discrimination of IRG and ORG systems in the Mazaruni Greenstone Belt, Guiana Shield, South America. South African Journal of Geology.
Kirk, J. D. (2004). Rhenium-osmium systematics of orogenic gold deposits through geologic time [Doctoral dissertation, University of Alberta]. ProQuest Dissertations & Theses Global.
Lowe, S. (2013). An epoch-based metallogenic scheme for northern Guyana: A tool for mineral resource assessment. West Indian Journal of Engineering, 35(2), 65-74.
Lowe, S. (2013). Potential for magmatic nickel-copper-platinum group element deposits (Ni-Cu-PGE) in northern Guyana. Caribbean Journal of Earth Science, 46, 43-50.
Tedeschi, M., & Hagemann, S. G. (2018). The Karouni gold deposit, Guyana, South America: Part II. Hydrothermal alteration and mineralization. Economic Geology, 113(8), 1705–1735.
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