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Flamenco: 2,200 ha Gollete: 27,200 ha Santa Bárbara: 44,000 ha

Strategic Location

“ Located in Highly mineralized San Juan Province, Argentina with several proven gold, silver and copper deposits.

Multi-Metal Systems - “Porphyry”

Targeting Au, Ag, Cu, Pb, Zn mineralization through Skarn, CRD, and Epithermal systems.

Unexplored Potential

Despite 50+ years of recognition none of our project has been drilled to date

STRATEGIC POSITIONING & KEY RESULTS

Geological Highlights

  • Porphyry Cu-Au system with extensive alteration halo.

  • Multiple mineralized centers identified by mapping and geochemistry.

  • Widespread phyllic and potassic alteration with local skarn development.

  • High-sulfidation epithermal overprint in select zones.

  • Limited historical drilling (shallow, peripheral to main targets).

Location within the Indio Belt

  • Strategic location in the Indio Belt, home to multi-million-ounce deposits.

  • Close analogues: Veladero (>15 Moz Au), Alturas (>6 Moz Au), and Salares Norte (>6.2Moz Au ).

  • Excellent access and infrastructure: year-round road access, camp nearby, water secured.

Located within the Indio-Pascual Belt
  • Indio Belt: Strategic position, host to multi-million-ounce deposits.
  • Close analogues: Veladero (>15 Moz Au), Alturas (>6 Moz Au), Salares Norte (>6.2 Moz Au).
  • Excellent infrastructure: year-round road access, nearby camp, water secured.
Indio Belt Regional Context
Schematic cross-section of the Gollete Project showing porphyry Cu-Au system, alteration zones (phyllic, potassic, skarn), and mineralized centers. Highlights include high-sulfidation epithermal overprint and limited historical drilling. GOLLETE

“El Indio belt has been the focus of over 30 years of exploration by many experienced explorers, resulting in a series of world class gold discoveries. These discoveries have evolved from outcropping high sulfidation towards semi-concealed deposits (Alturas, Veladero) reflecting the global trend towards concealed discoveries.”

Notable Geochemical Results (Surface Samples)

>412 ppm

As

0.13 g/t

Au

100 g/t

Ag

Anomalous

Sb, Hg, Ba

These high-grade values in surface samples confirm the presence of strong mineralization in the area.

Flamenco Project | Gold Mineralization

Flamenco

Project Highlights

  • Area: 2,200 hectares recently granted in well-known mineralized district
  • Distance: 5km from Gualcamayo Mine (7MOz Au mined)
  • Infrastructure: Excellent access and infrastructure available

This area shows strong potential for discovering gold, copper, lead, zinc, and silver mineralization related to Skarn, Distal Skarn, and CRD systems. Several key regional factors converge here, favoring gold deposition.

Geological Features

  • Strong Magnetic Feature Anomaly
  • Reactive Carbonate Host Rock (Ordovician)
  • Favorable Structural Setting (NE, NS, NW controls)
  • Historic Copper Mining presence
  • Strong Dickite-Kaolinite alteration
  • Advanced Argillic Alteration on site

Mineralization Potential

Strong potential for discovering gold, copper, lead, zinc, and silver mineralization related to:

  • Skarn Systems
  • Distal Skarn Systems
  • CRD (Carbonate Replacement Deposits)
  • Recent dating confirms ~19.5my age

Santa Barbara - New CRD District Discovery

Recent Discoveries

  • Chalcopyrite veins in limestone
  • Iron-rich limestone (bleached marble)
  • Strong geochemical anomalies
  • Controlled by Regional Thrust Faults
  • Marble–sulphide front extending 5 × 10 km
Santa Barbara Geology NEW

Cu: 1.5% in chalcopyrite veins in limestones
With: Hg, Sb, Mn, Ag >60ppm, U: 400ppm

Geochemical Anomalies

Cu
1.5%
Ag
60ppm
As
4,300ppm
Mo
2,500ppm

Field Observations

  • Hydrothermal Alteration: Clear, bleached marble front with abundant disseminated sulphides mapped across the area.
  • Structural Controls: Mineralization strongly controlled by NS, NW, and E–W structures with inverse thrust faulting.
  • Geological Setting: Much alteration/mineralization covered by Lomas de las Tapias Formation, suggesting later mineralizing event.

Cura Project

Geological Characteristics

  • Intermediate sulphidation system of >1.3km length
  • Epithermal system remains unexplored
  • Potentially extends below post-mineral volcanic rock
  • Strong argillic alteration observed
  • 1.5km extension with potential cover by post volcanics
  • Anomaly not followed up
Cura Project Geological Formation

Cura Project - Geological Field View

Geochemical Results

Significant mineralization values detected:

Zn
6.5%
Au
0.13g/t
Ag
15ppm
Mo
180ppm

UP TO 6.5% Zn, 0.13g/t Au and 15ppm Ag (Mo ~180ppm anomaly)

INTERMEDIATE SULPHIDATION STRUCTURE

CURA PROSPECT: UN-EXPLORED

Key Geological Features

  • STRONG ARGILLIC ALTERATION Indicative of intense, focused hydrothermal activity.
  • Geochemical Analysis
  • 1.5 km Extension Large-scale potential footprint for the mineralization.

Current Status & Recommendations

  • Possible Post-Volcanic Cover? Further analysis needed to confirm depth and extent of cover.
  • Anomaly Not Followed Up High-priority target requiring immediate trenching or drilling follow-up.
Geologists examining the Cura prospect trench with argillic alteration. Close-up of a rock sample showing intermediate sulphidation texture.
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