Mirasol staked the Sascha Project in 2003 which secured the Sascha Vein Zone. The 5 km-long Sascha Vein Zone was partially drill tested on the western end while under joint venture to Coeur Mining from 2006 to 2009. Two shallow holes were also drilled by Coeur at the Sasha Sur prospect. Coeur terminated the joint venture in 2009 and returned 100% of the project to Mirasol.
In early 2019, Mirasol signed an option to purchase agreement for the 5,700 ha Marcelina claims, consolidating the large prospective Sascha – Marcelina Low Sulfidation Epithermal (LSE) Au-Ag district under one company for the first time.
Mirasol can acquire 100% of the Marcelina claims from a privately-owned mining company, by making staged option payments totalling US$3.4 million over 4 years, with US$3.15 million due on the 4th anniversary. If the option is exercised, the Marcelina claims will be subject to a 1.5% NSR royalty. There is a minimum US$300,000 exploration spending commitment by Mirasol during the first three years of the option period.
The Sascha Marcelina Project is located 100 km south of Newmont Goldcorp’s Cerro Negro mine and displays similar geologic and geomorphic settings. Anomalous rock chip Au+Ag assays and Aster satellite alteration anomalies have defined a large-scale, zoned alteration system characteristic of an LSE Au+Ag system. Multiple, multi-kilometre long, mineralized vein and silicified breccia trends have been recognized across the project.
Mirasol’s surface exploration activities completed this last field season on the Sascha Marcelina project included geological mapping aided by the acquisition of drone supported high-resolution base images, detailed rock chip sampling, extensive soil grid sampling (with PXRF sourced geochemistry) and the acquisition of alteration data using in-house handheld ASD (Analytical Spectral Devices) technology on all of the rock chips and soil samples collected.
This work has defined a large alteration footprint of more than 20 km2, located in the immediate vicinity of the Marcelina claims, and hosting an epithermal silica vein system with multiple mineralized trends. Within this area, new prospects have been recognized, with the “Estancia Trend” and the “Igloo Trend”, both located in close proximity to an extensive silica cap (the “Pellegrini Silica Cap”), which is interpreted as representing the preserved fossil paleosurface of a low sulfidation system.
To date, a total of 422 new rock chip samples have been collected from within the Marcelina area with assays as high as 27.7 g/t Au and 121 g/t Ag, taken from epithermal silica vein/veinlets and silica-hematite hydrothermal breccias. These precious metal values are accompanied by highly elevated epithermal pathfinder elements including arsenic, antimony, tellurium, and anomalous lead and zinc. Strong positive correlations of key elements within the “epithermal suite” can be statistically recognized between gold, silver, arsenic and antimony.
In addition, Mirasol completed this field season additional surface exploration including a geophysics program at Sascha Marcelina. A total of 40 line-km of pole-dipole IP geophysics was completed over the three principle areas – the Estancia Trend (20.5 line-km), the Pellegrini silica cap (14.2 line-km) and the Igloo trend (5.35 line-km). Final processing and interpretations are pending. Mirasol will integrate these results, along with those from the recent mapping and sampling campaigns, to define drill targets all three prospects.
Mirasol is also making good progress in its search for a partner to drill test the project.
The Estancia Trend is represented by a NW trending structure hosting epithermal veins, veinlets and stockworks, which can be traced intermittently for more than 3 km through three principal outcropping zones identified as the Estancia South, Central and North zones.
The mineralization recognized within the Estancia South zone is emplaced into Chon Aike formation ignimbrites, which are known to be a permissive/brittle geological formation for mineralization in the Deseado Massif. This formation is interpreted to represent the deepest level of erosion with respect to the known geological stratigraphy mapped and hosts the most continuous and well-developed epithermal veins and veinlets with the highest gold and silver grades to date on the Marcelina claims. This suggests that the Estancia South zone is within or approaching the “productive level” of the mineralized epithermal column. The exposed mineralization at Estancia Central and North Zone, is hosted in the overlying La Matilde formation which is generally not considered to be an ideal host rock, although outcropping veinlets report highly anomalous gold values up to 1.86 g/t. Typically these values are hosted by irregular zones of stockworks and sheeted veinlets, which locally can form discrete bodies up to 20 m wide within the broader Estancia structural zone.
Interpretations based on the stratigraphic mapping, multi-element geochemistry, ASD alteration patterns and quartz silica species and textures suggest that both Estancia Central and North zones report to a higher level within the epithermal column. The Chon Aike formation, which is interpreted to underlie both the Central and North zones, is considered an attractive target for higher grade Au and Ag mineralization. It is also important to highlight that these mineralized trends disappear under post-mineral cover to both the south and north from their current mapped traces and are considered open along strike.
At Estancia South Zone, which represents the deepest part of the system recognized to date, good alteration zonation patterns are displayed within the outcropping epithermal veins. This zonation is interpreted to represent an increase in fluid temperature and proximity to fertile flow structures and to represent attractive targets for higher grade mineralization. This zonation is better developed in Estancia South due to the emplacement of hydrothermal fluids in the more brittle and competent Chon Aike Formation, that acted to concentrate the epithermal fluids in well-developed structures as opposed to being more dispersed through the flatter horizontal fluid outflow along the water table level as typically seen at the La Matilde Formation stratigraphic level.
The Pellegrini prospect is characterized by a large, high level “silica cap” comparable to Newmont Goldcorp’s Cerro Negro silica cap. This silica cap represents the highest level of epithermal paleo water table alteration hosted within the La Matilde Formation. It is uncommon for these upper levels of the epithermal column to be anomalous in precious metal concentrations, however, recent prospecting and sampling by Mirasol at Pellegrini encountered attractive epithermal textures in outcropping veins in close association with extensive NW oriented silicified breccia structures. These features are seen to cross-cut the high level silica cap alteration and may be associated with deeper feeder structures. Assays from these structures have returned values up to 1.95 g/t Au and 26.90 g/t Ag together with elevated values of arsenic, antimony, sulphur, copper, lead, tellurium and bismuth. These results are considered very encouraging, and further exploration will be designed to vector toward potential targets below the silica cap.
The interpretation of the exploration data to date suggests that the mineralization may also be related to a rhyolitic flow dome complex that has intruded into the upper levels of the La Matilde Formation in the central part of the Pellegrini prospect. This is coincident with a central sodium rich alunite zone which may represent a higher temperature/low pH response typical of advanced argillic alteration zones and may vector toward a possible NW feeder and/or hydrothermal up flow vent in this central part of the prospect. These observations are comparable to both the Cerro Saavedra zone at the Minera Santa Cruz’s San Jose mine and also Newmont Goldcorp’s Cerro Negro silica cap, both of which are located in reasonable proximity to the Sascha Marcelina project.
Recent rock chip sampling at the Igloo prospect have surpassed historical values previously reported, with peak assays up to 1.63 g/t Au, and 49.5 g/t Ag accompanied by anomalous arsenic, antimony, mercury and zinc, within hydrothermal breccia bodies developed in the La Matilde Formation. Mineralization also occurs as discontinuous quartz stockworks/veinlets which outcrop along a NW trending structural corridor. Recent geological/stratigraphic mapping suggests the more competent Chon Aike formation should shallowly underlie the La Matilde Formation, as seen in the Estancia South zone with the associated higher gold and silver values.