First Nordic Identifies New Multi-Kilometric Gold Anomaly and Returns Highest BoT Drilling Grades to Date at Paubäcken Project
- Discovery of Brokojan target – a large (2.3 km by 1 km) orogenic gold system multi-element pathfinder till anomaly; together with the adjacent Harpsund target, these two targets now form a large, semi-continuous southeast-northwest trending anomaly over a 5.5 km strike.
- Extension of bedrock anomalism along the Aida structural target by approximately 1 km, to 1.5 km now tested and confirmed for gold mineralization.
- Follow-up exploration programs planned in 2024 to continue to advance targets to drill testing stage.
3,050 regional B-Horizon (below topsoil) till samples were collected covering 1,350 hectares over a 12 km strike length of the northern extent of the first order Gold
For BoT sampling, two BoT samples from directly above the till bedrock interface and two bedrock samples within the top of bedrock are collected for all drill holes. All samples are screened with X-ray fluorescence ("XRF") and analysed using a multi-element suite at MSALABS in Storuman,
Results from the till sampling program have identified a second large gold pathfinder anomaly (Figure 2) northwest of the previously identified Harpsund 2.5 km by 1 km Au-As-Cu-Zn-Mo anomaly (gold-arsenic-copper-zinc-molybdenum) along the same structural corridor. Results from the till sampling program identified the Brokojan target, defined by a As-Cu-Zn-Mo pathfinder element till anomaly extending over 2.3 km by 1.0 km. The two targets now form a large, semi-continuous southeast-northwest trending anomaly over a 5.5 km strike of the Harpsund structural corridor. Both anomalies are oriented in the prominent ice flow direction. The survey focused on identification of orogenic gold and VMS (volcanogenic massive sulphide) type mineral systems known to be present in the Gold
The geology of the Harpsund target area (Figure 4) consists of a complex sequence of folded and sheared coarse to fine grained metasedimentary units that have been intruded by a series of felsic dykes and gabbroic units. The Harpsund structural corridor forms a southwest trending second order splay structure off the regional north-northwest trending Gold Line belt first order structure. The Harpsund target lies within the hinge of the second order structural corridor and the Brokojan target at the intersection of the first and second order structures. All sedimentary units demonstrate a dominant penetrative fabric and strong schistosity, and folding is isoclinal, indicating a high strain environment. Gold mineralized quartz veins previously mapped and sampled within the Harpsund target area are preferentially hosted within felsic dykes due to strong rheological contrast with surrounding metasediments.
Results from the BoT drilling program (Figure 5) were positive and extended anomalism along the Aida structural corridor to >1.5 km, including the highest BoT sample result todate on the Project, 5.01 g/t Au in hole PAU-23-BoT-065. The latest BoT drilling tested portions of the structure to the north and south of previous BoT and diamond drilling. The Aida structural corridor target lies under up to 25 m of glacial till cover and has been identified over 4 km in strike using magnetic geophysical data. Approximately 2.5 km of the target area remains completely untested, and the Company plans to continue target delineation BoT drilling activities in 2024.
Results from a sub-parallel structure zone were also positive with multiple bedrock samples encountered that are anomalous against background. The latest BoT program continues to demonstrate the size potential of the Aida target and follow up BoT drilling is planned for H2 2024 over the remaining untested 2.5 km strike of the structural corridor to develop targets for follow-up drill testing. The Aida target lies within 3.5 km of the past producing Svartliden gold mine, owned and operated by Dragon Mining Ltd ("Dragon"). The Svartliden mill and processing plant is still operational, and processes concentrate ore from Dragon's operations in
The geology of the Aida target consists of a sequence of isoclinal folded and sheared fine to course grained metasedimentary and metavolcanic units. The Aida structural corridor forms a 4 km long north-northwest trending second order structure sub-parallel to the regional first order Gold Line belt structure corridor. All units demonstrate a dominant penetrative fabric and schistosity, and folding is isoclinal, indicating a high strain environment. Mineralization is mainly hosted within the mafic volcanic and to a lesser extent coarser grained metagreywacke units that make up the foot wall. No mineralization is present within the finer grained black shale units that make up the hanging wall lithology. Mineralization is associated with arsenopyrite and both laminated and non-laminated quartz veins and has an affiliation to the highest strain zones of the mafic volcanic unit located at the footwall contact between the metavolcanic host and metagreywacke footwall units.
The Paubäcken project consists of three licenses totalling 17,097 ha that cover the central part of an emerging district in north central
The geology of the Gold Line belt consists of an inverted volcano-sedimentary sequence intruded by small pre- to syn-kinematic granitic intrusions within a broad, anastomosing high strain structural corridor. Lithologies are regionally metamorphosed to upper greenschist and amphibolite grade facies, and gold mineralization is associated with intense sericite, carbonate, biotite, and calc-silicate alteration assemblages and sulphide minerals pyrite, arsenopyrite, and pyrrhotite. The regional Gold Line structural corridor runs up the axis of the belt with many jogs, splays, and zones of structural complexity that are potential locations for dilation and deposition of gold bearing fluids. These lithological sequences are deemed to be highly prospective for orogenic gold deposits.
First Nordic's flagship is the Barsele gold project, located in
ON BEHALF OF THE BOARD OF DIRECTORS
President & CEO, Director
[1] Technical Report and Mineral Resource Estimate for the Barsele Property, 2020, InnovExplo
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This News Release contains forward-looking statements, including but not limited to comments regarding the timing and content of upcoming work programs, geological interpretations, receipt of property titles, potential mineral recovery processes, etc. Forward-looking statements address future events and conditions and therefore involve inherent risks and uncertainties. Actual results may differ materially from those currently anticipated in such statements and Barsele undertakes no obligation to update such statements, except as required by law.
APPENDIX
Figure
1
: Gold
Figure 2 : Map of Paubäcken project area showing regional till sampling geochemical results
Figure 3 : Map of Paubäcken project area showing historic ionic leach gold-in-till results
Figure 4 : Geological map of the Harpsund structural corridor
Figure 5 : Map of the Aida Target area showing BoT drilling results and recent extension of confirmed gold mineralization
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