CanAlaska Reports Significant Alteration In First Drill Program At Geikie Uranium Project

CanAlaska Reports Significant Alteration In First Drill Program At Geikie Uranium Project

Structurally Controlled Hydrothermal Alteration Associated with Faulted Graphitic Stratigraphy

Project Expanded by Staking 1,187 Hectares; Adding Priority Targets

CanAlaska Uranium Ltd. (TSXV: CVV) (OTCQX: CVVUF) (FSE: DH7N) ("CanAlaska or the "Company") is pleased to announce successful completion of the 2023 drill program at the Geikie project near the Athabasca Basin margin (Figure 1). The program focused on a 15-kilometre-long northeast trending conductor system with high-priority structural targets that were compiled from recent high-resolution airborne radiometric, magnetic, and electromagnetic surveys in combination with prospecting, structural mapping, and historical data review. The Company reports the objectives of the program were exceeded, identifying graphitic host rocks with large reactivated and brecciated fault zones, associated with hydrothermal alteration and elevated radioactivity.

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Figure 1 – Geikie Project Location
 
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2023 Geikie Summer Drill Program

The Geikie project is located approximately 10 kilometres east of the Athabasca Basin margin and 10 kilometres west of Highway 905. The 2023 summer drill program consisted of 2,217 metres in eight drill holes, representing CanAlaska's first drill holes on it's 60%-owned Geikie project. The program successfully intersected graphitic host rocks, showing evidence of multiple post-Athabasca structural reactivation events, associated with the intersection of north-south and northwest trending faults, hydrothermal alteration, and elevated radioactivity.

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Figure 2 – 2023 Geikie Drill Program Results
 
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The drill program confirmed the presence of hydrothermal alteration systems within a complex structural framework at Geikie, which is important in the formation of basement-hosted high-grade uranium deposits.

Results of this first drill program will allow for refinement of the exploration model on the Geikie project to target the most prospective portions of the multiple structural corridors. Significant early results from the Preston Creek target area indicates the 15-kilometre-long structural corridor represents a high priority target area for further drill testing (Figure 2).

Geochemical assay results for the 2023 program are pending.

2023 Geikie Summer Drill Program Target Area Results Summary

The Preston Creek target area is located at the northeastern end of the 15-kilometre-long conductor trend. Five drill holes (GKI004 - GKI008) were completed within this target area (Table 1). Each drill hole in this target area intersected re-activated basement faults, up to 30 metres in width, consisting of clay gouge and breccias within variably graphitic pelitic host rocks. Hydrothermal alteration enveloping the major fault zones consisted of hematite, chlorite, clay, and structurally-enhanced graphitic clays. Within the fault zones, the alteration intensifies and locally overprints the original host rock through numerous phases of faulting and fluid circulation (Figure 3). At the base of GKI004, an extensive zone of pervasive hematite alteration was intersected at the inferred contact between the Wollaston metasediments and Johnson Lake Granite. The 21-metre-thick interval was characterized by intense brick-red hematite completely overprinting the primary texture of the host rock. Abundant interstitial specular hematite and pyrite nodules were disseminated throughout the rock and as microfractures and fracture fillings. Additionally, in GKI005, elevated radiometry, up to 1,000 cps CT007-M, was intersected from 255.3 to 255.6 metres, associated with a sheared graphitic pelite. The complex structural framework of the Preston Creek target area with the associated hydrothermal alteration is very encouraging for the prospectivity of this portion of the 15-kilometre-long conductor trend and the broader project area.

The Aero Lake target area is located at the southern end of the 15-kilometre-long conductor trend. One drill hole (GKI 002) was completed within this target area (Table 1). GKI002 intersected a large re-activated fault zone from 59 to 88 metres characterized by cohesive breccias and cataclastic faults with dark grey clay gouge. Hydrothermal alteration spatially associated with the fault zone consists primarily of clay alteration and chloritization. At the base of GKI002, elevated radiometry, up to 1,750 cps CT007-M, is associated with semi-massive biotite in a pegmatite unit from 185.0 to 185.6 metres.

The Hourglass Lake target area is located midway along the 15-kilometre-long conductor trend. Two drillholes (GKI001 and GKI003) were completed within this target area (Table 1). Each drill hole intersected intervals of weakly to moderately graphitic pelite with only minor structural reactivation. The inferred offset of the conductor package identified from the VTEM survey has not yet been explained.

All reported depths and intervals are down hole depths and intervals, unless otherwise noted, and do not represent true thicknesses, which have yet to be determined.

CanAlaska CEO, Cory Belyk, comments, "The presence of large fault structures, hydrothermal alteration and elevated radiometric values is a great outcome from this first drilling program by CanAlaska and Basin Energy. The early drill results clearly indicate the right ingredients for basement-hosted uranium deposit formation are present and active on the Geikie project. This first exploration program has tested a very small portion of this very large project and there is very little doubt that further data analysis when assays are returned in conjunction with new geophysical data will yield additional high priority targets for the next phase of exploration."

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Figure 3 – Hydrothermal alteration enveloping fault zones in Preston Creek Target Area
 
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Geikie Project Expansion

The Geikie uranium project was recently expanded through claim staking to add two additional claims (Figure 2) totalling 1,187 hectares, now bringing the total Geikie project size to 35,084 hectares. The new claims are host to the historical Johnson Lake (Marina) Pb-Zn-Ag showing which consists of mineralization in outcrops, boulders, and drillholes. The mineralization occurs as disseminations, layers, and coarse pod-like segregations in addition to infills along fractures. Historical grab samples returned up to 5.31% Pb, 1.49% Zn, and 1.0 oz/t Ag. The additional claims have been added to the existing earn-in agreement between Basin Energy and CanAlaska.

Table 1 - 2023 Summer Drill Hole Collar Summary

Drill HoleTarget AreaEasting NorthingElevation
(m A.S.L.)
Azimuth (˚)Dip (˚)EOH (m)
GKI001Hourglass Lake5481576369438463.5130-60249.4
GKI002Aero Lake5458216366173446.0128-50240.5
GKI003Hourglass Lake5447436368493461.0130-50152.0
GKI004Preston Creek5511656372430450.5110-50390.0
GKI005Preston Creek5514246373287436.7122-45331.0
GKI006Preston Creek5521466375884462.0120-45310.0
GKI007Preston Creek5519776374956474.0120-45176.0
GKI008Preston Creek5512456372646433.6100-45368.0
Notes: Easting and Northing coordinates are reported in UTM Zone 13N (NAD83 datum). EOH = end of hole.
m A.S.L. = metres above sea level.

 

Geikie Project Overview

The Geikie Project is located just outside the eastern margin of the Athabasca Basin within the Wollaston Domain. The Project area has been subject to minimal exploration for uranium, with most significant work targeting base metals between 1967 and 1980. During this regional work, a series of mineralized showings were discovered in the Mud Lake and Johnson Lake South (Marina South) areas. The Mud Lake uranium-molybdenum showing recorded a series of anomalous rock chips with grades of up to 0.225%U, 5.2%Mo, and 1.4%Cu. The Johnson Lake South (Marina South) lead-zinc prospect recorded anomalous mineralization in outcrop of up to 2.03% Pb, 7.2% Zn and 0.93 oz/t Ag. Recent ground prospecting on the project has since confirmed the Mud Lake uranium-molybdenum, showing results with up to 3,250 ppm molybdenum total and 0.21% uranium total in grab samples.

The primary target on the Geikie project is basement-hosted uranium mineralization, where uranium bearing structures intersect favourable metasedimentary host rocks. The Geikie project is located within 10 kilometres of recent discoveries of basement-hosted uranium mineralization at the nearby Gemini Mineralized Zone ("GMZ") and ACKIO. These recent discoveries along with known mineralization at the nearby Agip-S and West Way prospects, all underscore the prospectivity of this portion of the Wollaston Belt.

The Geikie project is currently being sole-funded by Basin Energy Limited (ASX: BSN) under an option earn-in agreement with the Company.

Geochemical Sampling Procedures

All drill core samples from the 2023 program were shipped to the Saskatchewan Research Council Geoanalytical Laboratories (SRC) in Saskatoon, Saskatchewan. The samples were shipped in secure containment for preparation, processing, and multi-element analysis by ICP-MS and ICP-OES using total (HF:NHO3:HClO4) and partial digestion (HNO3:HCl), boron by fusion, and U3O8 wt% assay by ICP-OES using higher grade standards. Radiometric assay samples are chosen based on downhole probing radiometric equivalent uranium grades and scintillometer (SPP2 or CT007-M) peaks. Assay samples comprise 0.3 - 0.5 metre continuous split-core samples over the mineralized interval. A 0.1% U3O8 cut-off with a maximum internal dilution of 1 metre is used for compositing and reporting the data. The SRC is an ISO/IEC 17025/2005 and Standards Council of Canada certified analytical laboratory. Blanks, standard reference materials, and repeats are inserted into the sample stream at regular intervals by CanAlaska and the SRC in accordance with CanAlaska's quality assurance / quality control (QA/QC) procedures. Geochemical assay data are subject to verification procedures by qualified persons employed by CanAlaska prior to disclosure.

About CanAlaska Uranium

CanAlaska Uranium Ltd. (TSXV: CVV) (OTCQX: CVVUF) (FSE: DH7N) holds interests in approximately 350,000 hectares (865,000 acres), in Canada's Athabasca Basin - the "Saudi Arabia of Uranium." CanAlaska's strategic holdings have attracted major international mining companies. CanAlaska is currently working with Cameco and Denison at two of the Company's properties in the Eastern Athabasca Basin. CanAlaska is a project generator positioned for discovery success in the world's richest uranium district. The Company also holds properties prospective for nickel, copper, gold and diamonds. For further information visit www.canalaska.com.

The qualified technical person for this news release is Nathan Bridge, MSc., P.Geo., CanAlaska's Vice President, Exploration.

On behalf of the Board of Directors
"Cory Belyk"
Cory Belyk, P.Geo., FGC
CEO, President and Director
CanAlaska Uranium Ltd.

Contacts:

Cory Belyk, CEO and President
Tel: +1.604.688.3211 x 138
Email: cbelyk@canalaska.com

General Enquiry
Tel: +1.604.688.3211
Email: info@canalaska.com

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

Forward-looking information

All statements included in this press release that address activities, events or developments that the Company expects, believes or anticipates will or may occur in the future are forward-looking statements. These forward-looking statements involve numerous assumptions made by the Company based on its experience, perception of historical trends, current conditions, expected future developments and other factors it believes are appropriate in the circumstances. In addition, these statements involve substantial known and unknown risks and uncertainties that contribute to the possibility that the predictions, forecasts, projections and other forward-looking statements will prove inaccurate, certain of which are beyond the Company's control. Readers should not place undue reliance on forward-looking statements. Except as required by law, the Company does not intend to revise or update these forward-looking statements after the date hereof or revise them to reflect the occurrence of future unanticipated events.

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Forsys is pleased to provide an update for the Company's Norasa Uranium project ("Norasa 1 ") which comprises the deposits of Valencia Main and East, ("Valencia"), under Mining Licence (ML-149) and Namibplaas ("Namibplaas") under EPL-3638, (ML-251 pending).

Highlights

Forsys has undertaken a comprehensive review and update of all of the parameters for a Mineral Resource Estimate ("MRE") for the Norasa project using recent drill results together with the 2005-2011 previous MRE data. Confirmatory and geotechnical drilling, in conjunction with new survey information, including topographic surveys, down-the-hole optical televiewer surveys, trajectory surveys, and downhole gamma probe surveys, were used as inputs for mineral resource modelling. Re-interpretation of the previous database utilising all available data and modern estimation approaches has improved the definition of the MRE to more confidently support mine planning. This study, enhanced by an integrated and expanded drill program targeting existing and new areas together with a robust work plan of optimisation process testing and modelling, will help reinforce the upside potential of the Norasa project.

  • For the overall Norasa project, a conceptual pit constrained MRE for total deposits assessed from previous (2005-2011) and 2023 drilling results is estimated to be:
    • Valencia Main Measured and Indicated Resource at 40 ppm U 3 O 8 cutoff is estimated to be 152 Mt at 136 ppm eU 3 O 8 (equivalent U 3 O 8 ). Measured and Indicated contained metal is estimated at 45 Mlbs U 3 O 8 , at 40 ppm U 3 O 8 cutoff.
    • Valencia Main and East Inferred Resources are estimated at 5.7 Mt at 120 ppm eU 3 O 8 with 1.3 Mlbs U 3 O 8 contained metal oxide, at 40 ppm U 3 O 8 cutoff.
    • Namibplaas Inferred Resources are estimated to be 218.7 Mt at 85 ppm eU 3 O 8 with 41.1 Mlbs U 3 O 8 contained metal oxide, at 40 ppm U 3 O 8 cutoff.

Pine van Wyk, Country Director for Forsys commented: "The comprehensive work done over the last twelve months on the Norasa Uranium Project has created a solid foundation to advance project development.  The revised mineral resource model will help optimise the mine economics and process parameters. Results are expected soon from a column leaching test program currently being undertaken at SGS Laboratories in South Africa, which would establish the design basis of the planned heap leaching pads.  With the existing ML149 permitted to commence mining, the large scale Norasa project is well advanced to take advantage of the strong uranium sector fundamentals."

Mineral Resources
Results are reported from recent remodelling of historical (2005-2011) drilling and recent 2023 drilling results. The Mineral Resources are reported within US$120/lb U 3 O 8 pit shells, with a cut-off grade of 40 ppm U 3 O 8 for each of the deposits at Valencia Main and East, ("Valencia"), under Mining Licence (ML-149) and US$120/lb U 3 O 8 at 40 ppm U 3 O 8 cutoff at Namibplaas ("Namibplaas") under EPL-3638. The MRE are summarised as follows:

For the overall Norasa project, a conceptual open-pit shell constrained MRE for total deposits assessed from previous (2005-2011) and recent (2023) drilling results is estimated to be Measured and Indicated of 151.9 Mt at 136 ppm eU 3 O 8 , with contained metal oxide of 45.4 Mlbs U 3 O 8 at Valencia Main. Inferred Resources for the Norasa project are estimated to be 224.5 Mt at 86 ppm eU 3 O 8 , with contained metal oxide of 42.6 Mlbs U 3 O 8 (refer to Table 1):

  • Measured and Indicated: 151.9 Mt at 136ppm eU 3 O 8 , with contained metal oxide of 45.4 Mlbs for Valencia Main.
  • Inferred Resource for Valencia Main is estimated to be 4.7 Mt at 121 ppm eU 3 O 8 and 1.3 Mlbs eU 3 O 8 contained metal oxide.
  • Inferred Resource for Valencia East is estimated to be 1.0 Mt at 114 ppm eU 3 O 8 and 0.3 Mlbs U 3 O 8 contained metal oxide; and
  • Inferred Resource for Namibplaas is estimated to be 218.7 Mt at 85 ppm eU 3 O 8 and 41.1 Mlbs U 3 O 8 contained metal oxide.

Table 1: Mineral Resource Estimate for Norasa project as at 30 April 2024 at a 40 ppm U 3 O 8 cut-off grade.

Class Deposit Mass
Mt
(metric)
Average Grade
eU 3 O 8
(ppm)
Material Content
U 3 O 8
Mlbs
Contained Metal
U
tonnes
Measured Valencia East
Valencia Main 7.6 171 2.9 1,099
Namibplaas
Norasa 7.6 171 2.9 1,099
Indicated Valencia East
Valencia Main 144.3 134 42.6 16,368
Namibplaas
Norasa 144.3 134 42.6 16,368
Measured
&
Indicated
Valencia East
Valencia Main 151.9 136 45.4 17,467
Namibplaas
Norasa 151.9 136 45.4 17,467
Inferred Valencia East 1.0 114 0.3 97
Valencia Main 4.7 121 1.3 487
Namibplaas 218.7 85 41.1 15,817
Norasa 224.5 86 42.6 16,401


Notes:
1. All tabulated data have been rounded and as a result minor computational errors may occur.
2. Mineral Resources, which are not Mineral Reserves, have no demonstrated economic viability. There is no guarantee that all or any part of the mineral resource will be converted into a mineral reserve. The estimate of mineral resources may be materially affected by geology, environment, permitting, legal, title, taxation, socio-political, marketing, or other relevant issues.
3. The Mineral Resource Statement for Norasa as at 30th April 2024 is reported at a cut-off grade of 40ppm U 3 O 8 from within a conceptual pit-shell using the following assumed parameters:
  • Base Uranium Price –USD/lb U 3 O 8 : $120
  • Average Mining Cost at reference elevation (AISC) USD/tonne: Valencia Main $2.38; Valencia East $2.13; Namibplaas $2.29"
  • Average Processing Cost USD/tonne processed: $7.55
  • Average G&A Overheads USD/tonne processed: $1.04
  • Process Overall Recovery % U 3 O 8 Recovery: 85.0 %
  • Selling Cost Transport USD/lb U 3 O 8 : $1.29
4. From the assumed parameters, a 40 ppm U 3 O 8 cut-off grade was calculated, which together with the conceptual pit shell demonstrates reasonable prospects for eventual economic extraction (RPEEE) for the Mineral Resource. The assessment to satisfy the criteria of RPEEE is a high-level estimate and is not an attempt to estimate Mineral Reserves.

Mineral Resource Estimation Methodology

A summary of the Mineral Resource modelling methodology is as follows:

  • The Mineral Resource was modelled using a combination of Leapfrog Geo ® and Datamine Studio RM ® software.
  • Valencia Main and East data:
    • Comprise a combined dataset of 141 diamond (DD), 148 reverse circulation (RC) and 446 percussion (PC) type drill holes (Figure 1).
    • Borehole data from Valencia Main and East with XRF assay and calculated equivalent grades (eU 3 O 8 ) from gamma-probing for each of the deposits have been used to estimate the Mineral Resource.
    • Equivalent uranium grades have been factored to correlate practically well with the XRF data, which constitutes 25 % of the grade data.
    • Where XRF data are available these supercede the corresponding probe equivalent grade in the estimation data.
  • Namibplaas data:
    • Comprise a dataset of 530 percussion holes and 40 diamond drill holes (Figure 2).
    • Borehole data from Namibplaas XRF assay and calculated equivalent grades (eU 3 O 8 ) have been used to estimate the Inferred Mineral Resource.
    • Equivalent uranium grades constitute the majority of the grade data and where XRF data are available, ~3.5 % of all grade data, these supercede the probe derived values.
  • Wireframe interpretations of the logged lithologies were used to define the various geological units.
  • Mineralisation is strongly associated with alaskite intrusions, that are in turn controlled by a structural architecture that comprises folded and planar strata surfaces, and fold-associated shears and cleavages. Importantly, the orientation of marble strata is a major control on the distribution of uranium mineralisation for REDOX chemistry reasons, at Valencia and the Erongo region alaskite deposits as whole. The alaskite orientations are therefore strataform, except where they have invaded sheared and strongly cleaved antiformal hinge zones, as at Valencia Main. In order to honour the geological controls in the estimates various surfaces were modelled:
    • String interpretations of the "stratiform" intrusions were digitised in cross-section and were used to create median surfaces for each of the intrusions.
    • The resulting mineralised zone wireframes align with the lithological strata while also cross-cutting the strata in places to accommodate axial-planar mineralisation orientations (see Figure 3).
    • The surfaces were then used to guide the orientation of the grade estimate through interpolation of individual dip and dip directions for each model block.
  • The geometry of the Namibplaas deposit comprises stratiform lithologies that dip toward the southwest. The alaskite intrusives have intruded in a strataform manner and have exploited disruptions in the overall fabric, such as local fold flexures and dilation zones associated with the NE-SW regional extensional setting. In order to honour the geological controls at Namibplaas in the estimates various surfaces were modelled with guidance from the directions of greatest structural continuity to guide implicit modelling:
    • Along the strike and dip direction of the host metasediments, and
    • Along a shallow-plunging hinge structure that is oriented to the NE, parallel to the regional extension regime.
    • Considering that mineralization at Namibplaas is strongly associated with the granitic intrusions, string interpretations of the mid-points of these "stratiform" intrusions were digitized in cross-section, thereafter linked to create median surfaces of each of the alaskite intrusions (see Figure 4).
    • The surfaces of the intrusions were then used to guide the orientation of the grade estimate through interpolation of individual dip and dip directions for each model block.
  • Grade shells using a 40 ppm U 3 O 8 threshold were constructed using Leapfrog ® implicit modelling with directional control surfaces from the geological model.
  • The model volumes were divided into four domains at Valencia Main and two domains at Namibplaas. Each domain is distinct in terms of its geographic/geometric position as well as statistical / geostatistical parameters.
  • Ordinary kriging estimation used three-dimensional directional variograms to estimate U 3 O 8 grades within the mineralised zones for Valencia Main and Namibplaas. Inverse distance squared interpolation was used for Valancia East. The models underwent validation by comparison of estimated grade values against input sample grades, both visually and statistically.
  • Volumes covered by 30 m drill-spacing were classified as Indicated Mineral Resources at Valencia. All blocks outside of these volumes within the grade shells that received a grade estimate during the interpolation runs were considered Inferred.
  • At Namibplaas, although the tight drill spacing of approximately 30 m provides dense coverage of the deposit, the predominance of probe-derived eU 3 O 8 assays warrants a confidence level for an Inferred Resource.

30 April 2024 MRE block model and US$120/lb U3O8 pit shells at Valencia Main and Valencia East, ML 149.

Figure 1: 30 April 2024 MRE block model and US$120/lb U 3 O 8 pit shells at Valencia Main and Valencia East, ML 149.

30 April 2024 MRE block model and US$120/lb U3O8 pit shells at Namibplaas, EPL 3638.

Figure 2: 30 April 2024 MRE block model and US$120/lb U 3 O 8 pit shells at Namibplaas, EPL 3638.

Figure 3 part 1.Figure 3 part 2

Figure 3:  Shows the stacked concordant surfaces generated parallel to the 3 marble bands and orientation of mineralisation aligned with the strata and axial planar cleavages in the fold hinge (guiding surfaces hidden) at Valencia.

Shows alaskite midpoint strings (yellow) linked in parallel to the the NE-SW oriented strike of the deposit.

Figure 4:  Shows alaskite midpoint strings (yellow) linked in parallel to the the NE-SW oriented strike of the deposit.

In accordance with National Instrument 43-101 ("NI 43-101") a Technical Report outlining the mineral resource estimation will be filed under Forsys' profile on SEDAR+ ( www.sedarplus.ca ) within 45 days of the date of this release.

Assaying and QAQC

  • Recent (2023) Sampling and Assays
    • Samples were taken from the diamond drill cores and RC chips for geochemical assay guided by the routine downhole radiometric probe results, and sent to Trace Elements Analysis Laboratories (Pty) Ltd ("TEA Labs") at Swakopmund for sample preparation and analyses by XRF. For internal quality control purposes TEA Labs has weekly round robins with independent laboratories at Rosh Pinah, Swakop Uranium and Langer Heinrich mines.
    • Forsys employs a QAQC programme with Certified Reference Materials (CRMs), blanks, coarse duplicates and pulp duplicates inserted into each batch of samples. The QAQC insert rate comprises 4 % CRMs using three CRM types with different grades of U 3 O 8 ; 4 % blanks and 8 % to 10 % duplicates. RC sample batches have three types of duplicates; a field duplicate split at the drill rig; a coarse duplicate split at prescribed intervals at the laboratory; and pulp duplicates, also split at the laboratory. Core samples only have coarse and pulp duplicates split at the laboratory.
    • Four-percent of the samples sent to TEA Labs are sent for check analyses at SGS Laboratories (SGS) in South Africa, which serves as the independent accredited laboratory. The sample results are further validated by comparison with the radiometric scans.
  • Previous Sampling and Assays (2005-2011 Valencia Uranium Limited (VUL)):
    • All diamond drill half core and RC samples collected by VUL were assayed at the Setpoint Technology ("Setpoint") laboratory in Johannesburg, South Africa. Setpoint was accredited with the South African Accreditation System (SANAS), accreditation number T0223, and was also an ISO17025 accredited laboratory. Setpoint crushed and pulverised the samples for analysis of U 3 O 8 using the XRF pressed pellet method.
    • The VUL protocols for the QAQC were as follows:
      • CRMs inserted at a frequency of at least one per 20 samples.
      • Blanks inserted at a frequency of at least one per 50 samples.
      • Duplicates taken at a frequency of at least one per 20 samples.
    • The Setpoint laboratory included appropriate quality assurance and quality control (QAQC) procedures during the analysis of the VUL samples by including its own certified reference standards (CRM), blanks and duplicates.
    • VUL percussion holes were not physically sampled. Datasets were derived from two downhole probes that were calibrated against the XRF sample assays.
    • Snowden reviewed the assay results from Setpoint for the Valencia deposits in 2009 2 for the purposes of resource estimation and considered the QAQC results to be of a high standard of precision, unbiased and accurate.
    • Optiro reviewed the assay results from Setpoint for the Namibplaas deposit in 2011 and considered that the results of the QAQC indicate a high level of precision with no bias, no significant contamination and a high degree of accuracy (from Snowden 2009 2 and Optiro 2011 3 )
  • Trekkopje Exploration (Goldfields 1974-1984):
    • Exploration data derived from Trekkopje Exploration era, up to and including 1984, have not been verified by the QP and therefore were not utilised in this Mineral Resource Estimate.

Workplan

Forsys is undertaking an infill and extension drilling program and optimisation work with the aim of expanding and upgrading the Mineral Resource:

  1. Resource Infill Drilling and Resource Extension Drilling
    Total of 85 percussion drill holes for 7,520 metres have been laid out on a 25 x 25 metre grid. The objective is to more than double the quantity of the Measured Mineral Resource. The holes target the 660 m elevation with drill depths up to 100 m from surface and is comparable to the previous Measured Resource grid.

    A subsequent program for potential resource extension is planned for the areas adjacent to the Valencia Main deposit; along strike to the west, on the hinge zone to the south, and north of the Main deposit at the Jolie Zone.
  2. Pit Design Modeling
    The updated resource block model is used to assess open pit economic models. Pit slope design parameters are being reviewed to include lithological logging and geomechanical test work from additional drilling.
  3. Column Leaching Process Optimization Work
    Column Leach tests are presently underway at SGS in South Africa where the columns have been emptied and final analyses and data is pending. The next phase of testing will assess systematic processes to enhance the efficiency and effectiveness of extracting the uranium mineralisation from the ore using sulphuric acid solutions.
  4. Process Design
    DRA Global were appointed as the study contractor to deliver engineering to support preliminary cost estimates for a heap leach process. Ongoing engineering and optimisation continues.
  5. Bulk Sampling
    After site assessment and selection, a detailed plan is being drawn up to develop a box cut with the objective of retrieving approximately 20,000 tonnes of typical run-of-mine, fresh and representative sample material from the deposit.

Qualified Persons Statement for Metallurgy
Mr Aveshan Naidoo is a Specialist Engineer: Hydromet and Economics, for DRA South Africa Projects (Pty) Ltd of Building 33, Woodlands Office Park, 20 Woodlands Drive, Woodlands, Sandton, 2080. He holds a Bachelor of Science in Chemical Engineering and a Master of Business Administration at the University of Witwatersrand. He is a registered Professional Engineer with the Engineering Council of South Africa (Registration No. 20130523). Mr Naidoo has been practising his profession continuously since 2008 and has 16 years of experience across a range of African projects. He is familiar with NI 43-101 and, by reason of his education, experience, and professional registrations, he fulfils the requirements of an independent Qualified Person as defined in NI 43-101.

Qualified Persons Statement for Mineral Resource
The information in this release that relates to the updated Mineral Resource Estimate for the Norasa Project is based on information compiled or reviewed by Dr Guy Freemantle of The MSA Group (Pty) Ltd., Johannesburg, South Africa. The MSA Group are independent consultants to the Norasa Project, Namibia.  Dr Freemantle holds a Bachelor of Science in Geology and a PhD in Geology, both at the University of the Witwatersrand. He is a member of the Society of Economic Geologists (892905); a Fellow of the Geological Society of South Africa (965392); and is registered with SACNASP (Registration 117527). Dr Freemantle has practiced his profession continuously for 14 years and has sufficient experience and knowledge that is relevant to the style of mineralisation and type of deposits under consideration as well as to the activity that is being undertaken to fulfil requirements of a Qualified Person as per NI 43-101. Dr Freemantle consents to this release in the form and context in which it appears.

About Forsys Metals Corp.

Forsys Metals Corp. (TSX: FSY, FSE: F2T, NSX: FSY) is an emerging uranium developer focused on advancing its wholly-owned Norasa Uranium Project, located in the politically friendly jurisdiction of Namibia, Africa. The Norasa Uranium Project is comprised of the Valencia Uranium deposit (ML-149) and the nearby Namibplaas Uranium deposit (EPL-3638). Further information is available at the Company website www.forsysmetals.com

On behalf of the Board of Directors of Forsys Metals Corp. Richard Parkhouse, Director, Investor Relations.  For additional information please contact:

Pine van Wyk, Country Director, Forsys
email: pine@forsysmetals.com

Richard Parkhouse, Director, Investor Relations
email: rparkhouse@forsysmetals.com email: info@forsysmetals.com
phone : +44 7730493432

Nikolas Matysek,  Communications Manager (Canada)
email: nmatysek@forsysmetals.com

Forward Looking Statement

Certain information contained in this press release constitutes "forward-looking information" , within the meaning of Canadian legislation. Generally, these forward-looking statements can be identified by the use of forward-looking terminology such as "plans", "expects" or "does not expect", "is expected", "budget", "scheduled", "estimates", "forecasts", "intends", "anticipates" or "does not anticipate", or "believes", or variations of such words and phrases or state that certain actions, events or results "may", "could", "would", "might" or "will be taken", "occur", "be achieved" or "has the potential to". Forward looking statements contained in this press release are qualified in their entirety by the inherent risks and uncertainties surrounding future expectations. Among those factors which could cause actual results to differ materially are the following: market conditions and other risk factors listed from time to time in our reports filed with Canadian securities regulators on SEDAR at www.sedar+.com. The forward-looking statements included in this press release are made as of the date of this press release and Forsys Metals Corp disclaim any intention or obligation to update or revise any forward-looking statements, whether as a result of new information, future events or otherwise, except as expressly required by applicable securities legislation.

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  1. The election of the following nominees as directors of the Corporation for the ensuing year or until their successors are elected or appointed.

Votes ForVotes Withheld
              Catherine M. Best739,666,794
97.19%
21,395,027
2.81%
              M. Elizabeth Cannon755,414,889
99.26%
5,646,932
0.74%
              N. Murray Edwards734,115,206
96.46%
26,946,615
3.54%
              Christopher L. Fong730,264,360
95.95%
30,797,461
4.05%
              Ambassador Gordon D. Giffin681,630,086
89.56%
79,431,703
10.44%
              Wilfred A. Gobert749,993,920
98.55%
11,067,902
1.45%
              Christine M. Healy759,396,832
99.78%
1,664,989
0.22%
              Steve W. Laut752,522,642
98.88%
8,539,180
1.12%
              Honourable Frank J. McKenna713,843,507
93.80%
47,218,314
6.20%
              Scott G. Stauth755,136,229
99.22%
5,925,592
0.78%
              David A. Tuer721,224,440
94.77%
39,837,382
5.23%
              Annette M. Verschuren757,804,674
99.57%
3,257,147
0.43%




Votes ForVotes Withheld
  1. The appointment of PricewaterhouseCoopers LLP as auditors of the Corporation for the ensuing year and to authorize the Audit Committee of the Board of Directors to fix their remuneration.
733,200,212
94.14%
45,678,373
5.86%

Votes ForVotes Against
  1. Vote on Share Split of Issued and Outstanding Common Shares of the Corporation be subdivided on a two for one basis.
774,321,586
99.41%
4,556,996
0.59%

Votes ForVotes Against
  1. On an advisory basis, approval of the Corporation's approach to executive compensation.
748,228,501
98.31%
12,833,315
1.69%

 

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