Jucurutu Copper
A Region Renowned for its Favourable Copper Geology
Jucurutu Copper
Dive into the Jucuruto Copper Project and see what it has to offer
Overview
The Jucurutu Copper Project consists of 11 contiguous permit applications over 20,700 hectares in Rio Grande do Norte, Brazil—a region renowned for its favourable copper geology and proximity to major mining infrastructure. Anchored in the Caicó Complex and Seridó Group, the project stands out for its abundance of outcropping malachite showings and gossan-style weathering, indicating surface expressions of copper mineralization with significant continuity potential. Recent airborne geophysical surveys have confirmed compelling targets, while the nearby Suape port and the mining hub of Currais Novos offer unrivaled logistical advantages. Jucurutu is positioned to emerge as a flagship copper opportunity, looking to replicate the successes of Brazil’s productive Curaçá Valley and expand the nation’s critical mineral portfolio.
Key highlights for the jucurutu copper project
- Project Scale & Ownership: Eleven contiguous permit applications totaling 20,710 hectares in Rio Grande do Norte, acquired via ground staking, giving complete control over the exploration process.
- Prime Geological Setting: Located within the Caicó Complex (gneisses and migmatites) and Seridó Group (Jucurutu Formation, metasediments, quartzites, mica schists, metavolcanics, and marbles)—classic host lithologies for copper mineralization.
- Surface Mineralization: Multiple occurrences of malachite (oxide copper) showings and gossan-style weathering observed in the staked tenements; strong indicators for near-surface copper.
- Geophysical & Target Generation: Airborne magnetics have successfully delineated promising zones of copper mineralization, supporting focused ground follow-up.
- Infrastructure Advantage: Located just 200 km from Suape Port and 70 km from the well-established mining center of Currais Novos—facilitating access, logistics, workforce, and downstream processing options.
- Exploration Upside: No previous exploration in the tenement area ensures an untapped discovery opportunity, with recommendations to initiate detailed mapping, soil sampling, and ground geophysics upon claim granting.
- Benchmarking Potential: Geological and structural comparisons suggest the deposit style may mirror the renowned producing copper mines of Curaçá Valley, indicating robust upside.
ACQUISITION TERMS
100% Ownership via Ground Staking
Jucurutu Copper present work done
- Public airborne mag survey processing allowed the identification of potential copper mineralization and some malachite mineralized rocks were identified within the staked tenements.
Recommendations for work to be done in future:
Once the claims are granted, geological mapping, soil sampling and ground geophysics (magnetometry and IP) over the positive soil anomalies of copper.
Jucurutu Copper Geology
The Jucurutu region, has a geology characterized by the presence of the Caicó Complex and the Seridó Group, with the Jucurutu Formation standing out as the basal part of the group. The Caicó Complex is composed of gneisses and migmatites, while the Seridó Group includes formations such as Jucurutu, Equador, and others with metavolcanic rocks and marble.
Caicó Complex: Gneissic and migmatitic rocks predominate, representing a significant portion of the studied area.
Seridó Group: Jucurutu Formation: Represents the base of the group, with metasediments such as metaconglomerates, quartzites, and mica schists.
Equator Formation: Located between the Jucurutu Formation and other formations, it is composed of metaconglomerates and quartzites.
Other Formations: Include feldspathic and aluminous mica schists, with intercalations of metavolcanic rocks, marbles, and calc-silicate rocks.
Granitic rocks: Granitic rocks formed in the Neoproterozoic are also found, shaping the landscape and forming features such as inselbergs.
Jucurutu Copper Key features
Abundance of outcroping malachite showings and the presence of gosan style weathering.
