Genius Metals Secures an Option to Acquire a 100% Interest in a Prospective Copper-Gold Project in the Kingdom of Morocco

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Genius Metals Inc.
Genius Metals Inc.

MONTRÉAL, July 11, 2024 (GLOBE NEWSWIRE) -- Genius Metals Inc. (TSXV: GENI) ("Genius Metals" or the "Company") is pleased to announce that it has entered into an option agreement with Société Bleida Mineral Ressources SARL to acquire a 100% interest in the BMR Cu-Au project, located in the Kingdom of Morocco. This option agreement was negotiated at arm’s length. The Company aims to explore and develop the BMR project while continuing to advance its North American assets.

About the BMR Copper Property

The BMR Copper prospect covers an area of approximately 9 km² (Figure 1), located southeast of Ouarzazate. It is accessible via the national road N9, which connects the cities of Ouarzazate and Zagora, and by a 2 km track from kilometer 24 of road N9. The permit area, characterized by historical copper and manganese workings, comprises predominantly volcanic and volcano-clastic terrains of Ediacaran age. The property contains two main zones of mineralization with varying styles of copper mineralization.

To the south of the property a subvertical mineralized structure, with a 1.2 km strike length and up to 5m wide, is evidenced by the presence of a tectonic brecciation within a shear zone that is exposed at the surface. This structure is a brecciated quartz-carbonate vein with variable portions of chalcocite and malachite. The main zone of mineralization varies from 0.5m to 3m in width (locally reaching over a 5m width) and contains massive sulfide veins that dip steeply eastward (Figure 2). Initial surface sampling by Genius Metals from the exposed structure returned values up to 11.73% Cu and 5.53 g/t Au.

To the north of the property, there is a historical copper quarry from which approximately 4,000 tonnes of material were extracted, most of this material remains on the property. The copper mineralization in the northern part occurs in veins or is disseminated within the volcanic rocks (rhyolite and porphyritic rhyodacite). The mineralization is late to post-volcanic in age and appears to be controlled by magmatic and tectonic structures. A zone of propylitic alteration surrounds this mineralization.

An independent Canadian exploration consulting group is currently surface sampling exposed structures and trenches in order to test for copper mineralization and to also assess the gold potential, as the property has never been tested for gold.

Figure 1: Location of the BMR
Figure 1: Location of the BMR

Figure 1: Location of the BMR property and the two mineralized zones to the north and the south of the property


Figure 2: The main mineralized structure oriented N-S dipping eastward showing chalcocite and malachite
Figure 2: The main mineralized structure oriented N-S dipping eastward showing chalcocite and malachite


Figure 2: The main mineralized structure oriented N-S dipping eastward showing chalcocite and malachite