Summary
Results from an additional six holes of the ongoing drilling campaign have intersected broad zones of gold mineralization extending the strike length of the recent Kutuvuoma-Ikkari ('Helmi') Discovery to 1.3 km.
Aurion's JV partner,
0.71 g/t Au over 36.00 m from 32.10 m, including 3.08 g/t Au over 3.85 m, and 1.62 g/t Au over 9.66 m from 220.04 m in drill hole KUE21008, located approximately 800 m west of drill hole IKK21003. 5.50 m of core loss within the upper mineralized zone was assigned a value of zero.
Comments
'The Helmi discovery is already showing the potential to be a significant gold occurrence,' Commented Aurion CEO,
Additional broad zones of gold mineralization at Kutuvuoma-Ikkari Corridor
Six holes (total 1,434.6 m) of the 20 drill hole (total 5,201.5 m) program were drilled along an approximately 1 km long section of the Kutuvuoma-Ikkari structural corridor, to the west of hole IKK21003 (Helmi Discovery), which returned 1.84 g/t Au over 52.40 m. These holes were widely spaced, commencing approximately 270 m west of hole IKK21003 and 1.8 km west of
The Kutuvuoma-Ikkari corridor is an approximately 8 km long sequence of prospective geology along a domain boundary in the eastern part of the JV property extending from the Ikkari Discovery to the Kutuvuoma test pit.
The drill holes intersected metavolcanic and metasedimentary sequences and gabbro intrusions or sills. The mineralized intervals are mainly hosted in altered and sheared and/or brecciated mafic and ultramafic tuffs and tuffites with fine-grained pyrite as disseminations, interfolial sulphide or within narrow quartz-magnetite veins. The gold grades within the broader mineralized zones are relatively consistent.
IKK21004 was collared approximately 270 m northwest from drill hole IKK21003 that returned 1.84 g/t Au over 52.40 m. The hole intersected various lithologies of the Savukoski group including gabbro, talc-chlorite schist, mafic and ultramafic volcanics and sandstone of the Kumpu group. Foliated and altered (biotite, magnetite, sericite, carbonate, chlorite) mafic and ultramafic rocks contain broad zones of gold mineralization such as 0.64 g/t Au over 13.45 m from 51.45 and 0.87 g/t Au over 36.62 m from 75.78 m including 1.29 g/t Au over 19.90 m from 89.30 m.
IKK21005 was collared approximately 110 m west from IKK21004. The hole intersected various lithologies of the Savukoski group including gabbro, talc-chlorite schist, mafic and ultramafic volcanics and sandstone of the Kumpu group. Foliated and altered (biotite, magnetite, sericite, carbonate, chlorite) mafic and ultramafic rocks contain broad zones of gold mineralization such as 1.33 g/t Au over 9.15 m from 31.05 m including 2.89 g/t Au over 2.33 m, 0.62 g/t Au over 7.20 m from 43.00 m, 2.40 g/t Au over 0.96 m from 62.70 m, 1.70 g/t Au over 0.67 m from 104.53 m, 1.78 g/t Au over 0.93 m from 134.62 m and other zones with elevated (>0.1 g/t) gold values.
KUE21006 was collared approximately 360 m west-northwest from IKK21005. The hole intersected various lithologies of the Savukoski group including gabbro, diorite, talc-chlorite schist, mafic and ultramafic volcanics. The drill hole intersected intervals with anomalous (>0.1 g/t) gold values.
KUE21007 was collared approximately 70 m northwest from KUE21006. The hole intersected various lithologies of the Savukoski group including gabbro, diorite, intermediate volcanics and graphite bearing mudstones. Albite and sericite altered and brecciated zones of intermediate volcanics contain elevated gold values including 0.89 g/t Au over 3.20 m from 65.10 m. Elevated copper values up to 0.76% occur within the brecciated unit. Graphite bearing mudstones also contain elevated gold values in places including 0.90 g/t Au over 1.88 m from 179.65 m.
KUE21008 was collared approximately 200 m south from KUE21007 and 800 m west from IKK21003. The hole intersected various lithologies of the Savukoski group including talc-chlorite schist, mafic and ultramafic volcanics. Foliated or brecciated and altered (silicification, albite, sericite, carbonate) mafic and ultramafic rocks contain broad zones of gold mineralization such as 0.71 g/t Au over 36.00 m (5.50 of core loss assigned zero gold value) from 32.10 m including 3.08 g/t Au over 3.85 m (1.30 m of core loss assigned zero gold value) and 1.62 g/t Au over 9.66 m from 220.04 m.
KUE21009 was collared approximately 150 m west from KUE21008. The hole intersected various lithologies of the Savukoski group including talc-chlorite schist, mafic and ultramafic volcanics and sandstone of the Kumpu group. Foliated or brecciated and altered (silicification, biotite, chlorite, albite, sericite, carbonate) mafic and ultramafic rocks contain broad zones of gold mineralization such as 2.18 g/t Au over 1.77 m from 133.58 m, 2.55 g/t Au over 1.27 m from 161.30 m, 1.00 g/t Au over 4.24 m from 248.50 m and 2.29 g/t Au over 1.42 m from 259.00 m.
Broad zones of consistent gold mineralization have been identified in several holes over 1.3 km strike length along the prospective geological sequence between the Kutuvuoma test pit and the Ikkari Discovery highlighting the potential for the existence of gold mineralized system of scale along the 8 km long Kutuvuoma-Ikkari structural corridor of which the majority remains unexplored.
Aurion To Retain 30% Interest in the Joint Venture
Exploration activities in 2021
The JV is currently in the process of planning the 2022 exploration program.
About
Contact:
Tel: (416) 371-1325
Email: msantarossa@aurionresources.ca
(C) 2021 Electronic News Publishing, source