The principal mineral deposits in the Platosa area are high-temperature epigenetic silver leadzinc carbonate replacement deposits (CRD). The distal portions of these deposits are characterized by irregularly shaped pods, lenses, and roughly tabular or tubular masses of sulphide mineralization that can either cross-cut or run sub-parallel to the host stratigraphy. The near-vertical bodies are called chimneys, while the more horizontal and elongate masses are called mantos. Mantos and chimneys can extend for thousands of metres from the source of the mineralizing fluids and often follow tortuous paths through the host rocks. The distal massive sulphide bodies commonly grade progressively into mineralized metasomatic skarn deposits as source intrusions are approached. These intrusives are the ultimate source of CRD-type mineralization. This proximal mineralization includes skarns developed along fractures, along dyke and sill contacts, and as large irregular lenses on stock contacts. Locally, mineralized veins cut both the skarns and host intrusions. Metamorphic alteration (marbleization recrystallization, hornfels, and skarnoid) commonly occurs peripheral to the skarn zone. All aspects of CRD and skarn mineralization are locally and regionally structurally controlled. Important structural controls include faults, fractures, contacts, fold axes, and collapse (paleokarst) zones. Secondarily enhanced host rock permeability (i.e., fractures, breccias, solution cavities, dolomitization) is also an important controlling factor for mineralization (Megaw et al., 1988).

Mineralization at Platosa forms a series of mantos and chimneys localized at the intersection of the PSZ with a northeast striking lineament. As presently known, the bodies are found within an irregularly shaped 800 m by 700 m area. Most mantos dip gently to the east and are often connected by local, small chimney structures forming a stair-step pattern for a collective dip of 18º towards the east. Depth from surface ranges from 60 m in the west to over 315 m in the east. Sulphide mineralization is massive, banded, disseminated and fracture-filling, fineto coarse-grained galena and sphalerite, with minor accessory pyrite. The primary silver mineral is acanthite, which occurs as coarse blebs and fine-grained intergrowths with galena. Native silver and proustite occur locally. Silver, lead, and zinc grades are often high, especially in the more massive sections. Silver grades in the thousands of grams per tonne are not uncommon. Lead and zinc sulphides can constitute over 80% of the rock mass in drill core.

Drilling in the known manto area has also occasionally intersected anomalous copper and gold values, the gold occurring with the massive sulphides in several holes in the 6A Manto and in a siliceous/jasperoid zone overlying but some distance above portions of the NE1 Manto massive sulphides. Neither the copper nor gold is of sufficient continuity to be considered part of the Mineral Resource, however, its presence may be an indication of proximity to a mineralization plumbing system and this possibility is being studied. Gangue minerals include fine-grained calcite, coarse gypsum, quartz, and fluorescent purple fluorite.

Underground development has encountered several areas of lower grade, sulphide-rich breccias beneath and around many of the main sulphide bodies. These breccias are composed of coarse sulphide and wall rock fragments up to one metre in diameter, with interstices filled with loose to partially consolidated fine to coarse sulphide and dolomite sand. In many places, the infill shows the fine laminar bedding characteristic of cavern-fill sediments. These lowergrade zones may have formed through late intra-mineral to post-mineral dissolution of carbonate rocks around and below the mantos, with concurrent collapse of manto fragments and wall rocks into the voids, followed by later “washing” of finer-grained particles into the breccia voids by groundwater flow. Notably, the sand-sized fraction tends to be dominated by galena and/or acanthite and commonly yields high silver grades. In many places, these breccias are cross-cut and cemented by later gypsum deposition. Core recovery is often poor in the unconsolidated, sandier portions of these breccias.

A wide range of thermally metamorphosed rocks are found throughout the property. These include hornfels, skarnoid, and marble recrystallization of the carbonate host rocks. The heat source for the metamorphism is thought to be a polyphase intrusive body that may extend for several kilometres beneath the southwest flank of the Sierra Bermejillo. The extent of the body s revealed by regional aeromagnetic surveys flown by the Mexican Geological Survey and Excellon. Monzonite, granodiorite, granite, quartz-eye porphyry, and andesite porphyry have been found in isolated outcrops and drill holes throughout this area. Deeper holes drilled in this area have encountered copper-molybdenum-bearing veinlets and metasomatic skarn zones cutting the hornfels. Megaw (2002) postulated that these metamorphic and metasomatic fluids related to the deeper-seated portions of this intrusion were dammed below the relatively impermeable Lower Hornfels Formation and were only locally able to ascend into the upper carbonate units along faults and fractures.

The primary mining method has historically been a modified room and pillar, with the top of the manto being accessed first. For steeply dipping mantos, the area is benched down to a maximum height of 20 metres at which point a sill pillar is established. This process is repeated below the sill pillar until the bottom of the manto is reached. Historically, sill pillars were seldom necessary considering the flat- lying nature of the mantos, although these will become necessary where the mineralized body dips more steeply.

In 2018, Platosa transitioned the mining method to a cut and fill/drift and fill to increase the mining recovery. Engineering was completed for the construction of sill mattes composed of cemented rock fill (CRF) to eliminate the need for sill pillars in the future.

Primary stope accesses for cut-and-fill are driven into the deposit on a 15 percent decline. The bottom cut is mined, and the area is then backfilled with waste rock to facilitate extraction of the next cut. This
sequence is repeated up to five times until the stope access reaches an incline of 15 percent. Access to the next cut is then provided by a 15 percent decline driven from a higher elevation. The mine plan anticipates that the cut and fill stopes will be backfilled with unconsolidated development waste, except for where a sill matte will be required when mining will occur directly below. Development waste from active headings as well as waste that has been stockpiled underground will be used to backfill the cut and fill stopes.

Historical pillars are being extracted, with previously mined areas supported with cable bolts. Each area is evaluated individually based on the rock quality and economic viability.

The completion of the dewatering project has allowed Platosa to increase mechanization. Jacklegs have been replaced with jumbos in certain production areas, improving safety and productivity. Platform bolting drills were purchased in 2018 to improve the safety and productivity of installing ground support compared to current methods using handheld drills.

Mineralized material is hauled to surface using one 20-tonne haul truck and three 16-tonne haul trucks. The mineralized material is placed at surface at either the low-grade or high-grade stockpile. A wheel loader transfers the material from the stockpiles into the crusher; the material is then crushed to less than 25 millimetres. The crusher is equipped with a stacker conveyor that permits loading of the crushed material directly into haul trucks or can divert it on the ground if a truck is not available. The crushed material is hauled in 40-tonne covered trucks to the mineral processing facility located at Miguel Auza, 220 kilometres away.

There is currently no mineral processing carried out at the Platosa site. ROM material is crushed to minus 3/8 inch on site and, since mid-March 2009, has been processed at the Excellon-owned flotation mill in the town of Miguel Auza located 220 km south of the mine. The mill operates a conventional grinding/flotation/filtration circuit producing separate silverlead and silver-zinc concentrates. It has the capacity to process approximately 350 tpd of the high-grade Platosa mineralization with size of the flotation circuit being the limiting factor. This capacity exceeds the current mine production rate and, as a consequence, the mill operates on a variable schedule of several days on then several days off depending on mine and shipping schedules. Certain maintenance activities are carried out on the days the mill is not operating in order to minimize disruptions.

Production is crushed (to minus 3/8 in.) and hauled by truck from the Platosa Mine to the crushed ore storage are ........