It possibly consists of a VMS-type deposit located on levels of andesitic lavas with a porphyritic texture belonging to the Calipuy Group. The mineralization occurs in the form of mantles 10 to 20 meters thick with high values of copper and silver. The Project has currently been divided into three sectors: El Chilco Sector and Nueva Esperanza Sector and the Vetas Munchugo Sector that are currently under exploration.

Geologically, the Project is based on a sequence of sedimentary rocks, overlying volcanic rocks of the Calipuy Group, made up mainly of pyroclastics and lavas of andesitic composition. and  metallogenetically, the project is located on the limit of the strips of Au and Ag epithermal deposits, Cu, Mo and VMS porphyries.

Targets

The El Chilco Sector shows high geochemical anomalies with copper concentrations from 0.8% to 4% and silver values from 6 to 47 gr/T, accompanied by anomalous values in Mo, Ni, V, Pb and Zn.

In the Nueva Esperanza Sector, the mineralized structures show high concentrations of copper between 0.6 – 1.0%, accompanied by anomalous values of Bi, Mo, Ni, V, Pb and Zn.

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Within the mining property, it was possible to identify two important vein structures, with more than 1.5km of recognized structures divided into two main structures, the San Mateo vein being the most important because it contains the most important results in gold.

The San Mateo vein presents mineralization characteristics and favorable grades for small-scale mining activity, having more than 100 meters of outcrop and 200 meters of flare from the access road.

The location of the Pativilca de Oro mining concession is ideal from the mining point of view, since it is located 20 minutes from the North Pan-American highway, in addition to having relatively close water and electricity services, this makes the mining property an important factor. to take into account when evaluating future investments

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The Doña Elvira mine is located in the Crucero district, Carabaya province, Puno department.

Geology

The lithology is represented by greenish gray sandstones of the Tarma group. The mineralization is in veins and is made up of fine-grained galena, sphalerite, malachite and iron oxides, with a quartz gangue. The type of deposit is vein and in the form of a rosary.

Comments

The main vein has a strike of N10° W and a dip of 65°NE, being an irregular deposit. The power of the vein ranges from 0.40m to 1.20m. You can see a main work in a gallery that is approximately 50 meters long with a width of up to 2.5m. Currently there are no mining works.

Geochemistry

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