RISTI PROPERTY
RISTI PROPERTY
Aurion’s wholly owned Risti Property covers approximately 160 km2 in the CLGB in northern Finland. The Risti Property is located 20 km NNW of Sodankylä and is accessible via paved and all-weather gravel roads through rolling hills and forests.
Aurion has made multiple gold discoveries since the commencement of exploration activities in 2015. Significant new gold discoveries at Risti include: Aamurusko Main, Aamurusko NW, Notches, YNOT, A2 and Risti NW. The property also hosts the Kaaresselkä prospect discovered in the 1980s by the Geological Survey of Finland. Aurion’s pipeline of gold prospects at Risti are each at a different stage in the exploration process.
The geological setting of the Risti Property has many similarities to prolific gold-rich orogenic gold belts globally, such as the Timmins camp of the Abitibi region of Northern Ontario, Canada. The Aamurusko zone appears to be underlain by young unconformable clastic rocks (sandstones and conglomerates) of the Kumpu group. The Kumpu group conglomerates resemble the Timiskaming conglomerates of the Timmins and Kirkland Lake area of the Abitibi and occur in a similar geo-tectonic setting (both represent the youngest stratigraphic sequence within their respective belts). The Kumpu group and the Timiskaming group were deposited in late orogenic extensional basins. They form in relation to major movement along regional faults or deformation zones. In the Abitibi province, many high-grade, multi-million-ounce gold deposits are temporally and spatially associated with the Timiskaming conglomerates (or their equivalents) in close proximity to major regional deformation (fault) zones such as the Porcupine-Destor or Cadillac Lake-Larder Lake deformation zones. The Kumpu group appears to have been deposited in a similar geological setting adjacent to the Sirkka Shear Zone, the crustal scale deformation zone in the CLGB. Strong alteration including fuchsite, tourmaline, iron carbonate and albite associated with quartz veining and gold mineralization is seen along the entire length (>100 km) of this structure.
Gold is hosted by various lithologies including clastic conglomerates (examples: Aamurusko, Notches) and mafic-ultramafic rocks (examples: Ikkari, Kutuvuoma, Kaaresselkä) within the Risti Property and adjoining areas. The abundance and scale of gold mineralization along several structures over significant strike lengths and the fact that gold is hosted by various lithologies point to a conclusion that a powerful hydrothermal system has led to the camp scale footprint of gold mineralization.
The majority of the Risti Property had not been explored prior to Aurion. Aurion’s exploration activities started in 2015 with prospecting and mapping, which led to the initial discovery of high-grade boulders in the Aamurusko area in 2016. Further activities have included detailed and regional prospecting, geological mapping, trenching, ground and drone geophysics, soil sampling, base of till sampling and diamond core drilling.
| B2Gold JV | 298 | Ahvenjärvi, Hirvilavanmaa, Kettukuusikko, Kiekerömaa, Kutuvuoma, Kutuvuoma East, Palovaara, Sinermä, Soretialehto, Soretiavuoma, Tuongankuusikko |
|---|---|---|
| Kinross JV(*) | 90 | *On May 3, 2021, the Company received formal notice from Kinross that the option agreement has been terminated. Aurion will regain full ownership of the Property and related data. |
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Approximately 6,200 boulder, sub-crop and outcrop samples collected and assayed from the Risti Property average 6.7 g/t Au. The surface sampling has identified extensive footprints of gold mineralized samples in several areas including the Aamurusko and Notches prospects. The prospecting and mapping programs have mainly focused on domains with silica rich sediments, e.g. conglomerates, because such lithologies are comparably resistant to weathering and can be observed on surface in several areas. As such, sampling is mainly from gold mineralization hosted by clastic sediments. Mafic and ultramafic lithologies are less resistant to weathering and typically these areas are low lying and covered by overburden. Identification of this type of mineralization requires overburden penetrative exploration methods such as base of till sampling.
Exploration activities and results on various prospects are presented in the following chapters. Drill results presented herein are core lengths and may not represent true width. Channel sample results are surface channel cuts that also may not represent true width. Gold assay values are uncut. Prospecting grab samples may be selective and not representative of overall grade.