Gold: US $
Silver: US $
Zinc: US $
Copper: US $

Imiter bis (Ag, Au, Cu, Pb, Zn)

About Imiter bis

Imiter bis, formerly known as 233263 Permit, is an exploration property located on Morocco’s sub-Atlas range, about 150 kilometers from Ouarzazate and just five kilometers south of the world-class Imiter Mine. The geology and Phase I drill results indicate the presence of a 4-km potential at-surface polymetallic structure hosted within a low-sulphidation epithermal system




  • Ownership: 100%
  • One exploration permit covering 16 km²
  • Initial fieldwork: identification of a potential 4-km at-surface polymetallic structure (see left figure)
  • 2021: 4,380m scout drilling on 4 zones confirmed presence of gold and silver in several discovery holes
    • Vein system of >4km located close to major contact between granodiorite and main mafic dyke
    • Program confirmed continuity at depth with increasing widths in Middle Zone
  • 2022: 4,474m drill program following up on 2021 drill results and tested new area
    • Focus on 4 zones (Northwest, Daoud, Northeast-Extension and Dilatation Zones)
    • Encouraging results found in in the North Zone including 5.0m grading 3.94 g/t Au and 11.5m grading 1.46 g/t Au
    • H1-2022 airborne geophysical survey completed over 554 linear km
  • Follow-up drill programs will focus on finding the ‘boiling zone” with potential of richer mineralisation



The property is located in the Proterozoic Saghro “boutonnière” of Morocco’s Sub-Atlas range, about 150 kilometers from Ouarzazate and five kilometers south of the world-class Imiter Mine. Roads from Imiter village lead to the northern and southern ends of the property.



Imiter bis is underlain by a complex bi-modal volcanic sequence of the Ourzazate Supergroup overlying the Precambrian pelitic sequence of the Anti-Atlas Supergroup that hosts the Imiter silver deposit. The host bi-modal volcanic sequence consists of flow-banded rhyolite, felsic volcanic conglomerates, porphyritic dacite and andesite, and basalt. The host sequence is intruded by multiple syn-volcanic granitic and granodioritic intrusions and mafic dykes.

The property is cut by two major structures filled by low-sulphidation epithermal vein systems, oriented in a N-S and NE-SW orientation, associated with the regional fault system. Additionally, multiple syn-to-late-volcanic faults cut the sequence, many of which are mineralized.


Follow-up drill programs will focus on finding the ‘boiling zone” that could host higher-grade mineralization (see left figure).

The scientific and technical information contained on this page have been reviewed by David Lalonde, B. Sc, Head of Exploration, Qualified Person, for accuracy and compliance with National Instrument 43-101.



Discovery of trenches, small shafts and adits in several areas of the property.


Completion of IP/resistivity survey on permit centre
revealed 2 main geophysical domains


Completion of mapping, grab sampling, channel sampling and trenching.
Detailed ground MAG survey, and 4,062m of DDH drilling.


24 DDH for a total of 4,754m DDH, were conducted on 4 zones.
Targets informed by 2021 fieldwork and drilling, in addition to the 2022 airborne geophysical survey.