Drillhole WMA082-6 Intersected 9.6 metres at 14.9% U3O8 and Drillhole WMA082-4 Intersected 14.5 metres at 9.9% U3O8
Management Attending Investor Clubhouse at the RBC Open June 1, 2024
Vancouver, British Columbia--(Newsfile Corp. - May 29, 2024) - CanAlaska Uranium Ltd. (TSXV: CVV) (OTCQX: CVVUF) (FSE: DH7) ("CanAlaska" or the "Company") is pleased to report that it has received assay results from the drillholes completed on the Pike Zone during the winter of 2024. Geochemical assay results confirm composited high-grade intersections highlighted by WMA082-6 grading 14.9% U3O8 over 9.6 metres, and WMA082-4 grading 9.9% U3O8 over 14.5 metres. Drilling at the Pike Zone was completed as part of the ongoing winter exploration program on the West McArthur Joint Venture project (the "Project") in the eastern Athabasca Basin. The West McArthur project, a Joint Venture with Cameco Corporation, is operated by CanAlaska that holds an 83.35% ownership in the Project (Figure 1). CanAlaska is sole-funding the 2024 West McArthur program, further increasing its majority ownership in the Project.
CanAlaska CEO, Cory Belyk, comments, "Assay confirmation of the very high-grade uranium mineralization encountered at Pike Zone in the winter program is a critical step in evaluating the next steps for the project and the joint venture. The CanAlaska team will focus on expanding the known zone of unconformity-associated high-grade uranium during the upcoming summer drilling program scheduled to commence in early June. We remain confident Pike Zone is a potential tier one mineralizing event based on proven grade and thickness of uranium intersected at the unconformity, associated deep basement mineralized roots, and structure and alteration features observed in core at Pike Zone and elsewhere along the target corridor. Based on other eastern Athabasca Basin high-grade uranium deposit analogues such as McArthur River, Pike Zone could be just one of several pearls on a string."
2024 Winter Drill Program
The Company is pleased to announce completion of the 2024 winter drill program on the West McArthur project. The 2024 winter program was focused on continued expansion of the Pike Zone discovery and along strike unconformity testing to the northeast and southwest of the Pike Zone. During the drill program, eight unconformity target tests were completed for a total of 6,201 metres. All three drillholes (WMA082-4, WMA082-5, WMA082-6) completed on the Pike Zone intersected uranium mineralization. The mineralization in drillholes WMA082-4 and WMA082-6 represent the highest-grade mineralized intersections drilled to date on the West McArthur project.
Geochemical assay results confirm that drillhole WMA082-4 intersected one main composited interval of 7.4% U3O8 over 19.5 metres, including 9.9% U3O8 over 14.5 metres, followed by several additional mineralization intervals down hole (Table 1). The mineralization in WMA082-4 is characterized by massive to semi-massive, blebby, disseminated, clay-hosted, and fracture-controlled uranium mineralization associated with yellow and orange uranium secondaries at the contact between the Athabasca sandstone and the underlying basement rocks. The mineralized intervals are hosted within a broad zone of intense clay and chlorite alteration, resulting in complete replacement of the original rock fabric and textures. Intervals of no core recovery, due to poor ground conditions, were intersected within the WMA082-4 mineralized intersection. In intervals of no core recovery, downhole radiometric equivalent uranium grades, calculated based on an updated radiometric equivalent grade curve that has been correlated against geochemical assay results obtained during the winter drill program, are inserted in place of missing core and reported as part of the larger composited interval (Table 1).
Geochemical assay results confirm that drillhole WMA082-6 intersected one main composited interval of 12.9% U3O8 over 11.1 metres, including 14.9% U3O8 over 9.6 metres, followed by an additional mineralized interval down hole (Table 2). The mineralization in WMA082-6 is hosted directly at the unconformity contact between the Athabasca sandstone and the underlying basement rocks and is characterized by massive to semi-massive and nodular uranium mineralization associated with yellow and orange uranium secondaries and hematite alteration. Uranium mineralization continues into the basement rocks of WMA082-6 and is characterized by nodular, disseminated, clay-hosted, foliation-controlled, and fracture-controlled veinlets of uranium mineralization associated with localized pale-yellow uranium secondaries and strong basement alteration. One interval of no core recovery was intersected within the WMA082-6 mineralized intersection. In this interval of no core recovery, downhole radiometric equivalent uranium grades, calculated based on an updated radiometric equivalent grade curve that has been correlated against geochemical assay results obtained during the winter drill program, are inserted in place of missing core and reported as part of the larger composited interval (Table 2).
Geochemical assay results confirm that drillhole WMA082-5 intersected one interval of sandstone-hosted uranium mineralization grading 1.5% U3O8 over 4.6 metres (Table 3). The mineralization in WMA082-5 is located directly above the unconformity contact between the Athabasca sandstone and underlying basement rocks. The mineralization in WMA082-5 is characterized by disseminated and nodular uranium mineralization hosted within a dark grey to black sulfide- and clay-altered sandstone column with localized intervals of lost core due to high rock friability. The basement of WMA082-5 immediately below the unconformity is strongly clay and chlorite altered, resulting in replacement of the original rock fabric textures. One interval of no core recovery was intersected within the WMA082-5 mineralized intersection. In this interval of no core recovery, downhole radiometric equivalent uranium grades, calculated based on an updated radiometric equivalent grade curve that has been correlated against geochemical assay results obtained during the winter drill program, are inserted in place of missing core and reported as part of the larger composited interval (Table 3).
This most recent drill fence on the Pike Zone is located approximately 30 metres along strike to the northeast of high-grade uranium mineralization intersected in WMA082-2, which intersected 1.03% U3O8 over 6.3 metres, including a sub-interval of 2.82% U3O8 over 1.9 metres (see News Release dated January 18, 2024). Currently, the unconformity target at the Pike Zone remains open in all directions around WMA082-4, WMA082-5, and WMA082-6 (Figure 2).
2024 Summer Drill Program and Next Steps
The Company is actively planning the 2024 summer drill program on the West McArthur project. The drill program is expected to start in early June and will consist of two diamond drills targeting approximately 9,000 metres of additional diamond drilling. The program is expected to be completed by September.
In addition, the Company has retained the services of Understood Mineral Resources Ltd ("Understood") of Saskatoon. With the assistance of Understood, the Company has generated an updated radiometric probe equivalent grade curve utilizing the geochemical assay confirmed intersections from the Pike Zone. This updated radiometric probe equivalent curve, which factors in the ultra high-grades intersected during the winter drill program, will allow for better defined equivalent uranium calculations of potential future high-grade intersections. Understood will also be providing the Company with geostatistical-based resource modelling services in preparation for a potential future resource calculation on the Pike Zone.
Table 1 - WMA082-4 Intersections with Geochemical Assay and Radiometric Equivalent Intervals
| WMA082-4 Intervals 1 | From
(m) | To
(m) | Length
(m)7 | Average Grade
|
| (% U3O8) | (% eU3O8)8 |
| Interval 1 (2) | 796.5 | 797.0 | 0.5 | | 0.20 |
| 797.0 | 797.3 | 0.3 | 1.4 | |
| 797.3 | 799.0 | 1.7 | | 2.1 |
| 799.0 | 802.2 | 3.2 | 30.9 | |
| 802.2 | 803.0 | 0.8 | | 3.6 |
| 803.0 | 808.5 | 5.5 | 3.6 | |
| 808.5 | 809.5 | 1.0 | | 9.8 |
| 809.5 | 812.5 | 3.0 | 2.4 | |
| 812.5 | 814.0 | 1.5 | | 0.9 |
| 814.0 | 816.0 | 2.0 | 0.2 | |
| Composited Interval 1 (2,3) | 796.5 | 816.0 | 19.5 | 7.4 | |
| Including (4) | 797.0 | 797.3 | 0.3 | 1.4 | |
| Including (3,5) | 798.5 | 813.0 | 14.5 | 9.9 | |
| | | | | | |
| Interval 2 (6) | 822.6 | 827.5 | 4.9 | 0.9 | |
| Including (4) | 822.6 | 823.9 | 1.3 | 1.9 | |
| Including (4) | 824.7 | 825.2 | 0.5 | 2.3 | |
| | | | | | |
| Interval 3 (6) | 829.6 | 831.6 | 2.0 | 0.4 | |
- WMA082-4 was drilled at an azimuth of 295 ̊ with an inclination of -79.3 ̊, collared at 477,345 mE / 6,396,525 mN, 605 m A.S.L. (UTM NAD83 Z13N).
- Intersection interval is composited above a cut-off grade of 0.1% U3O8 / eU3O8 with a maximum of 1.0 m of internal dilution.
- Composited intervals contain geochemical assay where core was recovered, and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
- Intersection interval is composited above a cut-off grade of 1.0% U3O8 with a maximum of 1.0 m of internal dilution.
- Intersection interval is composited above a cut-off grade of 1.0% U3O8 / eU3O8 with a maximum of 1.0 m of internal dilution.
- Intersection interval is composited above a cut-off grade of 0.1% U3O8 with a maximum of 1.0 m of internal dilution.
- All reported depths and intervals are drill hole depths and intervals, unless otherwise noted, and do not represent true thicknesses, which have yet to be determined.
- Radiometric equivalent ("eU3O8") derived from a calibrated downhole gamma probe. No core was recovered within these intervals and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
|
Table 2 - WMA082-6 Intersections with Geochemical Assay and Radiometric Equivalent Intervals
| WMA082-6 Intervals 1 | From
(m) | To
(m) | Length
(m)6 | Average Grade
|
| (% U3O8) | (% eU3O8)7 |
| Interval 1 (2) | 798.0 | 800.5 | 2.5 | | 16.7 |
| 800.5 | 809.1 | 8.6 | 11.9 | |
| Composited Interval 1 (2,3) | 798.0 | 809.1 | 11.1 | 12.9 | |
| Including (4) | 798.9 | 808.5 | 9.6 | 14.9 | |
| | | | | | |
| Interval 2 (5) | 815.9 | 816.6 | 0.7 | 0.7 | |
- WMA082-6 was drilled at an azimuth of 295 ̊ with an inclination of -79.3 ̊, collared at 477,345 mE / 6,396,525 mN, 605 m A.S.L. (UTM NAD83 Z13N).
- Intersection interval is composited above a cut-off grade of 0.1% U3O8 / eU3O8 with a maximum of 1.0 m of internal dilution.
- Composited intervals contain geochemical assay where core was recovered, and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
- Intersection interval is composited above a cut-off grade of 1.0% U3O8 / eU3O8 with a maximum of 1.0 m of internal dilution.
- Intersection interval is composited above a cut-off grade of 0.1% U3O8 with a maximum of 1.0 m of internal dilution.
- All reported depths and intervals are drill hole depths and intervals, unless otherwise noted, and do not represent true thicknesses, which have yet to be determined.
- Radiometric equivalent ("eU3O8") derived from a calibrated downhole gamma probe. No core was recovered within these intervals and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
|
Table 3 - WMA082-5 Intersections with Geochemical Assay and Radiometric Equivalent Intervals
| WMA082-5 Intervals 1 | From
(m) | To
(m) | Length
(m)5 | Average Grade
|
| (% U3O8) | (% eU3O8)6 |
| Interval 1 (2) | 804.3 | 805.0 | 0.7 | | 0.15 |
| 805.0 | 808.9 | 3.9 | 1.7 | |
| Composited Interval 1 (2,3) | 804.3 | 808.9 | 4.6 | 1.5 | |
| Including (4) | 806.4 | 808.4 | 2.0 | 3.2 | |
- WMA082-5 was drilled at an azimuth of 295 ̊ with an inclination of -79.3 ̊, collared at 477,345 mE / 6,396,525 mN, 605 m A.S.L. (UTM NAD83 Z13N).
- Intersection interval is composited above a cut-off grade of 0.1% U3O8 / eU3O8 with a maximum of 1.0 m of internal dilution.
- Composited intervals contain geochemical assay where core was recovered, and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
- Intersection interval is composited above a cut-off grade of 1.0% U3O8 with a maximum of 1.0 m of internal dilution.
- All reported depths and intervals are drill hole depths and intervals, unless otherwise noted, and do not represent true thicknesses, which have yet to be determined.
- Radiometric equivalent ("eU3O8") derived from a calibrated downhole gamma probe. No core was recovered within these intervals and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
|
Other News
The Company will have management representatives at the Investor Clubhouse at the RBC Open on June 1, 2024 in Hamilton, Ontario.
Geochemical Sampling Procedures and Use of Radiometric Equivalent Grades
All drill core samples from the 2024 program were shipped to the Saskatchewan Research Council Geoanalytical Laboratories (SRC) in Saskatoon, Saskatchewan 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. Assay samples are chosen based on downhole probing radiometric equivalent uranium grades and scintillometer (SPP2 or CT007-M) peaks. Assay sample intervals comprise 0.3 - 0.8 metre continuous half-core split samples over the mineralized interval. Select density samples, comprising 0.1 metre continuous whole core samples that are subsequently split and assayed, may be taken within the mineralized interval. With all assay samples, one half of the split sample is retained and the other sent to the SRC for analysis. 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.
During active exploration programs drillholes are radiometrically logged using calibrated downhole GeoVista NGRS and TGGS (Triple GM) gamma probes which collect continuous readings along the length of the drillhole. Preliminary radiometric equivalent uranium grades ("eU3O8") are then calculated from the downhole radiometric results. The probe is calibrated using an algorithm calculated from the calibration of the probe at the Saskatchewan Research Council facility in Saskatoon and from the comparison of probe results against geochemical analyses. At extremely high radiometric equivalent uranium grades, downhole gamma probes may become saturated, resulting in the probe being overwhelmed, which in turn can create difficulties in accurately determining extremely high-grade radiometric equivalent uranium grades. The equivalent uranium grades are preliminary and are subsequently reported as definitive assay grades following sampling and chemical analysis of the mineralized drill core. In the case where core recovery within a mineralized intersection is poor or non-existent, radiometric grades are considered to be more representative of the mineralized intersection and may be reported in the place of assay grades. Radiometric equivalent probe results are subject to verification procedures by qualified persons employed by CanAlaska prior to disclosure.
All reported depths and intervals are drill hole depths and intervals, unless otherwise noted, and do not represent true thicknesses, which have yet to be determined.
About CanAlaska Uranium
CanAlaska Uranium Ltd. (TSXV: CVV) (OTCQX: CVVUF) (FSE: DH7) holds interests in approximately 500,000 hectares (1,235,000 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 on the West McArthur JV project and Denison on the Moon Lake South JV project 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 .
The Qualified Person under National Instrument 43-101 Standards of Disclosure for Mineral Projects for this news release is Nathan Bridge, MSc., P. Geo., Vice-President Exploration for CanAlaska Uranium Ltd., who has reviewed and approved its contents.
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: +1.306.668.6900
Email: cbelyk@canalaska.com
General Enquiry
Tel: +1.306.668.6915
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.
Drillhole WMA082-6 Intersected 9.6 metres at 14.9% U3O8 and Drillhole WMA082-4 Intersected 14.5 metres at 9.9% U3O8
WMA082-6 鑽孔在 U14.9% 處相交 9.6 米3O8 而且 Drillhole WMA082-4 在 9.9% U處相交 14.5 米3O8
Management Attending Investor Clubhouse at the RBC Open June 1, 2024
管理層在2024年6月1日的加拿大皇家銀行公開賽上參加投資者俱樂部會所
Vancouver, British Columbia--(Newsfile Corp. - May 29, 2024) - CanAlaska Uranium Ltd. (TSXV: CVV) (OTCQX: CVVUF) (FSE: DH7) ("CanAlaska" or the "Company") is pleased to report that it has received assay results from the drillholes completed on the Pike Zone during the winter of 2024. Geochemical assay results confirm composited high-grade intersections highlighted by WMA082-6 grading 14.9% U3O8 over 9.6 metres, and WMA082-4 grading 9.9% U3O8 over 14.5 metres. Drilling at the Pike Zone was completed as part of the ongoing winter exploration program on the West McArthur Joint Venture project (the "Project") in the eastern Athabasca Basin. The West McArthur project, a Joint Venture with Cameco Corporation, is operated by CanAlaska that holds an 83.35% ownership in the Project (Figure 1). CanAlaska is sole-funding the 2024 West McArthur program, further increasing its majority ownership in the Project.
不列顛哥倫比亞省溫哥華--（Newsfile Corp.-2024 年 5 月 29 日）- 加拿大阿拉斯加鈾業有限公司（多倫多證券交易所股票代碼：CVV） (OTCAX: CVVUF) (FSE: DH7) （“CanAlaska” 或 “公司”）很高興地報告說，它已經收到了2024年冬季在派克區完成的鑽孔的化驗結果。地球化學分析結果證實了以 WMA082-6 分級爲重點的複合高等級交叉點 14.9%3O8 超過 9.6 米，以及 WMA082-4 分級 上漲9.9％3O8 超過 14.5 米。作爲阿薩巴斯卡盆地東部的西麥克阿瑟合資企業項目（“項目”）正在進行的冬季勘探計劃的一部分，派克區的鑽探已經完成。西麥克阿瑟項目是與Cameco公司的合資企業，由Canalaska運營，該公司持有該項目83.35％的所有權（圖1）。Canalaska正在爲2024年西麥克阿瑟計劃提供獨家資金，進一步增加了其在該項目中的多數股權。
CanAlaska CEO, Cory Belyk, comments, "Assay confirmation of the very high-grade uranium mineralization encountered at Pike Zone in the winter program is a critical step in evaluating the next steps for the project and the joint venture. The CanAlaska team will focus on expanding the known zone of unconformity-associated high-grade uranium during the upcoming summer drilling program scheduled to commence in early June. We remain confident Pike Zone is a potential tier one mineralizing event based on proven grade and thickness of uranium intersected at the unconformity, associated deep basement mineralized roots, and structure and alteration features observed in core at Pike Zone and elsewhere along the target corridor. Based on other eastern Athabasca Basin high-grade uranium deposit analogues such as McArthur River, Pike Zone could be just one of several pearls on a string."
CanAlaska 首席執行官科裏·貝利克評論說， “通過化驗確認冬季項目在派克區遇到的極高品位鈾礦化是評估該項目和合資企業下一步行動的關鍵步驟。在計劃於6月初開始的夏季鑽探計劃中，Canalaska團隊將重點擴大已知的不合格相關高品位鈾區域。我們仍然相信，派克區是潛在的一級礦化事件，這是基於在不整合處相交的鈾的經過驗證的等級和厚度、相關的深層基底礦化根系，以及在派克區和目標走廊沿線其他地方觀察到的岩心結構和蝕變特徵。基於阿薩巴斯卡盆地東部其他高品位鈾礦牀類似物，例如麥克阿瑟河，派克區可能只是幾顆珍珠中的一顆。”
2024 Winter Drill Program
The Company is pleased to announce completion of the 2024 winter drill program on the West McArthur project. The 2024 winter program was focused on continued expansion of the Pike Zone discovery and along strike unconformity testing to the northeast and southwest of the Pike Zone. During the drill program, eight unconformity target tests were completed for a total of 6,201 metres. All three drillholes (WMA082-4, WMA082-5, WMA082-6) completed on the Pike Zone intersected uranium mineralization. The mineralization in drillholes WMA082-4 and WMA082-6 represent the highest-grade mineralized intersections drilled to date on the West McArthur project.
該公司很高興地宣佈，西麥克阿瑟項目的2024年冬季鑽探計劃已經完成。2024年冬季計劃的重點是繼續擴大派克區的發現範圍，並將罷工不合格測試擴展到派克區的東北和西南部。在鑽探計劃中，共完成了八項不合格目標測試，總長度爲6,201米。在派克區完成的所有三個鑽孔（WMA082-4、WMA082-5、WMA082-6）都與鈾礦化區相交。WMA082-4 和 WMA082-6 鑽孔中的礦化是迄今爲止在西麥克阿瑟項目上鑽探的最高品位的礦化交叉點。
Geochemical assay results confirm that drillhole WMA082-4 intersected one main composited interval of 7.4% U3O8 over 19.5 metres, including 9.9% U3O8 over 14.5 metres, followed by several additional mineralization intervals down hole (Table 1). The mineralization in WMA082-4 is characterized by massive to semi-massive, blebby, disseminated, clay-hosted, and fracture-controlled uranium mineralization associated with yellow and orange uranium secondaries at the contact between the Athabasca sandstone and the underlying basement rocks. The mineralized intervals are hosted within a broad zone of intense clay and chlorite alteration, resulting in complete replacement of the original rock fabric and textures. Intervals of no core recovery, due to poor ground conditions, were intersected within the WMA082-4 mineralized intersection. In intervals of no core recovery, downhole radiometric equivalent uranium grades, calculated based on an updated radiometric equivalent grade curve that has been correlated against geochemical assay results obtained during the winter drill program, are inserted in place of missing core and reported as part of the larger composited interval (Table 1).
地球化學分析結果證實，WMA082-4 鑽孔與一個 7.4% 的鈾的主要複合間隔相交3O8 超過 19.5 米，包括 9.9%3O8 超過 14.5 米，隨後在井下還有幾個額外的礦化間隔（表 1）。WMA082-4 中的礦化特徵是塊狀到半塊狀、氣泡狀、瀰漫性、粘土狀和裂縫控制的鈾礦化，與阿薩巴斯卡砂岩與底層基底巖接觸處的黃色和橙色二級鈾有關。礦化間隔位於粘土和亞氯酸鹽強烈蝕變的廣闊區域內，從而完全取代了原有的岩石結構和紋理。由於地質條件不佳，沒有岩心回收的間隔在 WMA082-4 礦化交叉點內相交。在沒有岩心回收的間隔內，根據更新的輻射等效品位曲線計算得出的井下輻射當量鈾等效品位曲線，該曲線與冬季鑽探計劃期間獲得的地球化學分析結果相關，被插入缺失岩心並作爲更大綜合間隔的一部分進行報告（表 1）。
Geochemical assay results confirm that drillhole WMA082-6 intersected one main composited interval of 12.9% U3O8 over 11.1 metres, including 14.9% U3O8 over 9.6 metres, followed by an additional mineralized interval down hole (Table 2). The mineralization in WMA082-6 is hosted directly at the unconformity contact between the Athabasca sandstone and the underlying basement rocks and is characterized by massive to semi-massive and nodular uranium mineralization associated with yellow and orange uranium secondaries and hematite alteration. Uranium mineralization continues into the basement rocks of WMA082-6 and is characterized by nodular, disseminated, clay-hosted, foliation-controlled, and fracture-controlled veinlets of uranium mineralization associated with localized pale-yellow uranium secondaries and strong basement alteration. One interval of no core recovery was intersected within the WMA082-6 mineralized intersection. In this interval of no core recovery, downhole radiometric equivalent uranium grades, calculated based on an updated radiometric equivalent grade curve that has been correlated against geochemical assay results obtained during the winter drill program, are inserted in place of missing core and reported as part of the larger composited interval (Table 2).
地球化學分析結果證實，WMA082-6 鑽孔與一個 12.9% 的鈾的主要複合間隔相交3O8 超過 11.1 米，包括 14.9% 的鈾3O8 超過 9.6 米，隨後在井下還有一個額外的礦化間隔（表 2）。WMA082-6 中的礦化直接存在於阿薩巴斯卡砂岩與下層基底岩石之間的不整合接觸處，其特徵是與黃色和橙色鈾次級礦化以及赤鐵礦蝕變相關的塊狀到半塊狀鈾礦化。鈾礦化延伸到 WMA082-6 的基底岩石中，其特徵是鈾礦化的結核狀、浸染、粘土託管、葉片控制和裂縫控制的礦脈，與局部的淡黃色鈾次生礦和強烈的基底變化有關。在 WMA082-6 礦化交叉點內有一段沒有岩心回收的間隔。在這段沒有岩心回收的間隔內，根據更新的輻射等效品位曲線計算得出的井下輻射當量鈾等效品位曲線，該曲線與冬季鑽探計劃期間獲得的地球化學分析結果相關，被插入缺失岩心並作爲更大綜合間隔的一部分進行報告（表2）。
Geochemical assay results confirm that drillhole WMA082-5 intersected one interval of sandstone-hosted uranium mineralization grading 1.5% U3O8 over 4.6 metres (Table 3). The mineralization in WMA082-5 is located directly above the unconformity contact between the Athabasca sandstone and underlying basement rocks. The mineralization in WMA082-5 is characterized by disseminated and nodular uranium mineralization hosted within a dark grey to black sulfide- and clay-altered sandstone column with localized intervals of lost core due to high rock friability. The basement of WMA082-5 immediately below the unconformity is strongly clay and chlorite altered, resulting in replacement of the original rock fabric textures. One interval of no core recovery was intersected within the WMA082-5 mineralized intersection. In this interval of no core recovery, downhole radiometric equivalent uranium grades, calculated based on an updated radiometric equivalent grade curve that has been correlated against geochemical assay results obtained during the winter drill program, are inserted in place of missing core and reported as part of the larger composited interval (Table 3).
地球化學分析結果證實，WMA082-5 鑽孔與一個間隔的砂岩託管鈾礦化區相交，鈾礦化等級爲 1.5%3O8 超過 4.6 米（表 3）。WMA082-5 中的礦化位於阿薩巴斯卡砂岩與底層岩石之間的不整合接觸點正上方。WMA082-5 中的礦化特徵是浸染鈾和結核鈾礦化位於深灰色至黑色硫化物和粘土變化的砂岩柱中，由於岩石脆性高，岩石易碎性高，岩心會出現局部丟失間隔。不合格之處正下方的 WMA082-5 基底被強烈的粘土和亞氯酸鹽改變，導致原來的岩石織物紋理被取代。在 WMA082-5 礦化交叉點內有一段沒有岩心回收的間隔。在這段沒有岩心回收的間隔內，根據更新的輻射等效品位曲線計算得出的井下輻射當量鈾等效品位曲線，該曲線與冬季鑽探計劃期間獲得的地球化學分析結果相關，被插入缺失岩心並作爲更大綜合間隔的一部分進行報告（表3）。
This most recent drill fence on the Pike Zone is located approximately 30 metres along strike to the northeast of high-grade uranium mineralization intersected in WMA082-2, which intersected 1.03% U3O8 over 6.3 metres, including a sub-interval of 2.82% U3O8 over 1.9 metres (see News Release dated January 18, 2024). Currently, the unconformity target at the Pike Zone remains open in all directions around WMA082-4, WMA082-5, and WMA082-6 (Figure 2).
派克區的最新鑽探圍欄位於與 WMA082-2 相交的高品位鈾礦化區走向東北約 30 米處，該礦化區與 1.03% 的鈾相交3O8 超過 6.3 米，包括 2.82% U 的子間隔3O8 超過 1.9 米（參見 2024 年 1 月 18 日的新聞稿）。目前，派克區的不合格目標在 WMA082-4、WMA082-5 和 WMA082-6 周圍的各個方向上仍然是開放的（圖 2）。
2024 Summer Drill Program and Next Steps
The Company is actively planning the 2024 summer drill program on the West McArthur project. The drill program is expected to start in early June and will consist of two diamond drills targeting approximately 9,000 metres of additional diamond drilling. The program is expected to be completed by September.
該公司正在積極規劃西麥克阿瑟項目的2024年夏季演習計劃。鑽探計劃預計將於6月初開始，將包括兩臺金剛石鑽機，目標是再鑽探約9,000米。該計劃預計將於9月完成。
In addition, the Company has retained the services of Understood Mineral Resources Ltd ("Understood") of Saskatoon. With the assistance of Understood, the Company has generated an updated radiometric probe equivalent grade curve utilizing the geochemical assay confirmed intersections from the Pike Zone. This updated radiometric probe equivalent curve, which factors in the ultra high-grades intersected during the winter drill program, will allow for better defined equivalent uranium calculations of potential future high-grade intersections. Understood will also be providing the Company with geostatistical-based resource modelling services in preparation for a potential future resource calculation on the Pike Zone.
此外，該公司還保留了薩斯卡通明德礦產資源有限公司（“Underseded”）的服務。在Understeed的協助下，該公司利用經地球化學分析確認的來自派克區的交叉點，生成了更新的輻射探測器等效等級曲線。這條更新的輻射探測器當量曲線考慮了冬季鑽探計劃期間相交的超高等級探測器等效曲線，將允許對未來潛在的高品位交叉點進行更明確的當量鈾計算。Unfersed還將爲公司提供基於地統計學的資源建模服務，爲未來可能在派克區進行資源計算做準備。
Table 1 - WMA082-4 Intersections with Geochemical Assay and Radiometric Equivalent Intervals
表 1-含地球化學分析和輻射等效間隔的 WMA082-4 交叉點
|
WMA082-4 Intervals 1
|
From
(m)
|
To
(m)
|
Length
(m)7
|
Average Grade
|
|
(% U3O8)
|
(% eU3O8)8
|
| Interval 1 (2)
|
796.5 |
797.0 |
0.5 |
|
0.20 |
| 797.0 |
797.3 |
0.3 |
1.4 |
|
| 797.3 |
799.0 |
1.7 |
|
2.1 |
| 799.0 |
802.2 |
3.2 |
30.9 |
|
| 802.2 |
803.0 |
0.8 |
|
3.6 |
| 803.0 |
808.5 |
5.5 |
3.6 |
|
| 808.5 |
809.5 |
1.0 |
|
9.8 |
| 809.5 |
812.5 |
3.0 |
2.4 |
|
| 812.5 |
814.0 |
1.5 |
|
0.9 |
| 814.0 |
816.0 |
2.0 |
0.2 |
|
|
Composited Interval 1 (2,3)
|
796.5 |
816.0 |
19.5 |
7.4 |
|
|
Including (4)
|
797.0 |
797.3 |
0.3 |
1.4 |
|
|
Including (3,5)
|
798.5 |
813.0 |
14.5 |
9.9 |
|
| |
|
|
|
|
|
| Interval 2 (6)
|
822.6 |
827.5 |
4.9 |
0.9 |
|
|
Including (4)
|
822.6 |
823.9 |
1.3 |
1.9 |
|
|
Including (4)
|
824.7 |
825.2 |
0.5 |
2.3 |
|
| |
|
|
|
|
|
| Interval 3 (6)
|
829.6 |
831.6 |
2.0 |
0.4 |
|
- WMA082-4 was drilled at an azimuth of 295 ̊ with an inclination of -79.3 ̊, collared at 477,345 mE / 6,396,525 mN, 605 m A.S.L. (UTM NAD83 Z13N).
- Intersection interval is composited above a cut-off grade of 0.1% U3O8 / eU3O8 with a maximum of 1.0 m of internal dilution.
- Composited intervals contain geochemical assay where core was recovered, and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
- Intersection interval is composited above a cut-off grade of 1.0% U3O8 with a maximum of 1.0 m of internal dilution.
- Intersection interval is composited above a cut-off grade of 1.0% U3O8 / eU3O8 with a maximum of 1.0 m of internal dilution.
- Intersection interval is composited above a cut-off grade of 0.1% U3O8 with a maximum of 1.0 m of internal dilution.
- All reported depths and intervals are drill hole depths and intervals, unless otherwise noted, and do not represent true thicknesses, which have yet to be determined.
- Radiometric equivalent ("eU3O8") derived from a calibrated downhole gamma probe. No core was recovered within these intervals and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
|
|
WMA082-4 間隔 1
|
來自
(m)
|
到
(m)
|
長度
(m)7
|
平均成績
|
|
(% U)3O8)
|
(% 歐盟3O8)8
|
| 間隔 1 (2)
|
796.5 |
797.0 |
0.5 |
|
0.20 |
| 797.0 |
797.3 |
0.3 |
1.4 |
|
| 797.3 |
799.0 |
1.7 |
|
2.1 |
| 799.0 |
802.2 |
3.2 |
30.9 |
|
| 802.2 |
803.0 |
0.8 |
|
3.6 |
| 803.0 |
808.5 |
5.5 |
3.6 |
|
| 808.5 |
809.5 |
1.0 |
|
9.8 |
| 809.5 |
812.5 |
3.0 |
2.4 |
|
| 812.5 |
814.0 |
1.5 |
|
0.9 |
| 814.0 |
816.0 |
2.0 |
0.2 |
|
|
複合間隔 1 (2,3)
|
796.5 |
816.0 |
19.5 |
7.4 |
|
|
包括 (4)
|
797.0 |
797.3 |
0.3 |
1.4 |
|
|
包括 (3,5)
|
798.5 |
813.0 |
14.5 |
9.9 |
|
| |
|
|
|
|
|
| 間隔 2 (6)
|
822.6 |
827.5 |
4.9 |
0.9 |
|
|
包括 (4)
|
822.6 |
823.9 |
1.3 |
1.9 |
|
|
包括 (4)
|
824.7 |
825.2 |
0.5 |
2.3 |
|
| |
|
|
|
|
|
| 間隔 3 (6)
|
829.6 |
831.6 |
2.0 |
0.4 |
|
- WMA082-4 鑽探的方位角爲 295，傾角爲 -79.3，鑽孔爲 477,345 mE/6,396,525 mN，A.S.L. 605 米（UTM NAD83 Z13N）。
- 交叉間隔在截止等級高於 0.1% U 時合成3O8 /歐盟3O8 最大內部稀釋量爲 1.0 m。
- 複合間隔包含回收岩心的地球化學分析，並插入井下輻射等效鈾等效等效品位來代替缺失的岩心間隔。
- 交叉間隔的合成比例高於 1.0% U 的截止等級3O8 最大內部稀釋量爲 1.0 m。
- 交叉間隔的合成比例高於 1.0% U 的截止等級3O8 /歐盟3O8 最大內部稀釋量爲 1.0 m。
- 交叉間隔在截止等級高於 0.1% U 時合成3O8 最大內部稀釋量爲 1.0 m。
- 除非另有說明，否則所有報告的深度和間隔均爲鑽孔深度和間隔，並不代表尚未確定的真實厚度。
- 輻射當量（“eU”3O8“) 源自經過校準的井下伽瑪探測器。在這些間隔內沒有發現任何岩心，用井下輻射等效鈾等級來代替缺失的岩心間隔。
|
Table 2 - WMA082-6 Intersections with Geochemical Assay and Radiometric Equivalent Intervals
表 2-含地球化學分析和輻射等效間隔的 WMA082-6 交叉點
|
WMA082-6 Intervals 1
|
From
(m)
|
To
(m)
|
Length
(m)6
|
Average Grade
|
|
(% U3O8)
|
(% eU3O8)7
|
| Interval 1 (2)
|
798.0 |
800.5 |
2.5 |
|
16.7 |
| 800.5 |
809.1 |
8.6 |
11.9 |
|
|
Composited Interval 1 (2,3)
|
798.0 |
809.1 |
11.1 |
12.9 |
|
|
Including (4)
|
798.9 |
808.5 |
9.6 |
14.9 |
|
| |
|
|
|
|
|
| Interval 2 (5)
|
815.9 |
816.6 |
0.7 |
0.7 |
|
- WMA082-6 was drilled at an azimuth of 295 ̊ with an inclination of -79.3 ̊, collared at 477,345 mE / 6,396,525 mN, 605 m A.S.L. (UTM NAD83 Z13N).
- Intersection interval is composited above a cut-off grade of 0.1% U3O8 / eU3O8 with a maximum of 1.0 m of internal dilution.
- Composited intervals contain geochemical assay where core was recovered, and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
- Intersection interval is composited above a cut-off grade of 1.0% U3O8 / eU3O8 with a maximum of 1.0 m of internal dilution.
- Intersection interval is composited above a cut-off grade of 0.1% U3O8 with a maximum of 1.0 m of internal dilution.
- All reported depths and intervals are drill hole depths and intervals, unless otherwise noted, and do not represent true thicknesses, which have yet to be determined.
- Radiometric equivalent ("eU3O8") derived from a calibrated downhole gamma probe. No core was recovered within these intervals and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
|
|
WMA082-6 間隔 1
|
來自
(m)
|
到
(m)
|
長度
(m)6
|
平均成績
|
|
(% U)3O8)
|
(% 歐盟3O8)7
|
| 間隔 1 (2)
|
798.0 |
800.5 |
2.5 |
|
16.7 |
| 800.5 |
809.1 |
8.6 |
11.9 |
|
|
複合間隔 1 (2,3)
|
798.0 |
809.1 |
11.1 |
12.9 |
|
|
包括 (4)
|
798.9 |
808.5 |
9.6 |
14.9 |
|
| |
|
|
|
|
|
| 間隔 2 (5)
|
815.9 |
816.6 |
0.7 |
0.7 |
|
- WMA082-6 鑽探的方位角爲 295，傾角爲 -79.3，鑽孔爲 477,345 mE/6,396,525 mN，A.S.L. 605 米（UTM NAD83 Z13N）。
- 交叉間隔在截止等級高於 0.1% U 時合成3O8 /歐盟3O8 最大內部稀釋量爲 1.0 m。
- 複合間隔包含回收岩心的地球化學分析，並插入井下輻射等效鈾等效等效品位來代替缺失的岩心間隔。
- 交叉間隔的合成比例高於 1.0% U 的截止等級3O8 /歐盟3O8 最大內部稀釋量爲 1.0 m。
- 交叉間隔在截止等級高於 0.1% U 時合成3O8 最大內部稀釋量爲 1.0 m。
- 除非另有說明，否則所有報告的深度和間隔均爲鑽孔深度和間隔，並不代表尚未確定的真實厚度。
- 輻射當量（“eU”3O8“) 源自經過校準的井下伽瑪探測器。在這些間隔內沒有發現任何岩心，用井下輻射等效鈾等級來代替缺失的岩心間隔。
|
Table 3 - WMA082-5 Intersections with Geochemical Assay and Radiometric Equivalent Intervals
表 3-含地球化學分析和輻射等效間隔的 WMA082-5 交叉點
|
WMA082-5 Intervals 1
|
From
(m)
|
To
(m)
|
Length
(m)5
|
Average Grade
|
|
(% U3O8)
|
(% eU3O8)6
|
| Interval 1 (2)
|
804.3 |
805.0 |
0.7 |
|
0.15 |
| 805.0 |
808.9 |
3.9 |
1.7 |
|
|
Composited Interval 1 (2,3)
|
804.3 |
808.9 |
4.6 |
1.5 |
|
|
Including (4)
|
806.4 |
808.4 |
2.0 |
3.2 |
|
- WMA082-5 was drilled at an azimuth of 295 ̊ with an inclination of -79.3 ̊, collared at 477,345 mE / 6,396,525 mN, 605 m A.S.L. (UTM NAD83 Z13N).
- Intersection interval is composited above a cut-off grade of 0.1% U3O8 / eU3O8 with a maximum of 1.0 m of internal dilution.
- Composited intervals contain geochemical assay where core was recovered, and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
- Intersection interval is composited above a cut-off grade of 1.0% U3O8 with a maximum of 1.0 m of internal dilution.
- All reported depths and intervals are drill hole depths and intervals, unless otherwise noted, and do not represent true thicknesses, which have yet to be determined.
- Radiometric equivalent ("eU3O8") derived from a calibrated downhole gamma probe. No core was recovered within these intervals and downhole radiometric equivalent uranium grades are inserted in place of missing core intervals.
|
|
WMA082-5 間隔 1
|
來自
(m)
|
到
(m)
|
長度
(m)5
|
平均成績
|
|
(% U)3O8)
|
(% 歐盟3O8)6
|
| 間隔 1 (2)
|
804.3 |
805.0 |
0.7 |
|
0.15 |
| 805.0 |
808.9 |
3.9 |
1.7 |
|
|
複合間隔 1 (2,3)
|
804.3 |
808.9 |
4.6 |
1.5 |
|
|
包括 (4)
|
806.4 |
808.4 |
2.0 |
3.2 |
|
- WMA082-5 鑽探的方位角爲 295，傾角爲 -79.3，鑽孔爲 477,345 mE/6,396,525 mN，A.S.L. 605 米（UTM NAD83 Z13N）。
- 交叉間隔在截止等級高於 0.1% U 時合成3O8 /歐盟3O8 最大內部稀釋量爲 1.0 m。
- 複合間隔包含回收岩心的地球化學分析，並插入井下輻射等效鈾等效等效品位來代替缺失的岩心間隔。
- 交叉間隔的合成比例高於 1.0% U 的截止等級3O8 最大內部稀釋量爲 1.0 m。
- 除非另有說明，否則所有報告的深度和間隔均爲鑽孔深度和間隔，並不代表尚未確定的真實厚度。
- 輻射當量（“eU”3O8“) 源自經過校準的井下伽瑪探測器。在這些間隔內沒有發現任何岩心，用井下輻射等效鈾等級來代替缺失的岩心間隔。
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The Company will have management representatives at the Investor Clubhouse at the RBC Open on June 1, 2024 in Hamilton, Ontario.
公司將於2024年6月1日在安大略省漢密爾頓舉行的加拿大皇家銀行公開賽的投資者俱樂部派出管理層代表。
Geochemical Sampling Procedures and Use of Radiometric Equivalent Grades
All drill core samples from the 2024 program were shipped to the Saskatchewan Research Council Geoanalytical Laboratories (SRC) in Saskatoon, Saskatchewan 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. Assay samples are chosen based on downhole probing radiometric equivalent uranium grades and scintillometer (SPP2 or CT007-M) peaks. Assay sample intervals comprise 0.3 - 0.8 metre continuous half-core split samples over the mineralized interval. Select density samples, comprising 0.1 metre continuous whole core samples that are subsequently split and assayed, may be taken within the mineralized interval. With all assay samples, one half of the split sample is retained and the other sent to the SRC for analysis. 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.
2024 年計劃中的所有鑽芯樣本均運送到位於薩斯喀徹溫省薩斯卡通的薩斯喀徹溫省研究委員會地質分析實驗室 (SRC)，採用總量 (Hf: nho3: HCL) 和部分消化 (HnO3: HCL)、聚變硼和鈾進行製備、處理和多元素分析，由 ICP-MS 和 ICP-OES 進行製備、處理和多元素分析3O8 ICP-OES 使用更高級別的標準對 wt% 進行測定。化驗樣本是根據井下探測的輻射等效鈾等級和閃爍計（SPP2 或 CT007-M）峯值來選擇的。化驗樣本間隔包括礦化間隔內 0.3-0.8 米的連續半核分裂樣品。選擇的密度樣本，包括0.1米連續的整個岩心樣本，隨後進行分割和分析，可以在礦化間隔內採集。對於所有化驗樣本，保留一半的拆分樣本，另一半發送到SRC進行分析。SRC 是經過 ISO/IEC 17025/2005 和加拿大標準委員會認證的分析實驗室。根據Canalaska的質量保證/質量控制（QA/QC）程序，CanAlaska和SRC定期將空白、標準參考材料和重複樣本插入樣本流。在披露之前，地球化學分析數據必須經過Canalaska僱用的合格人員的驗證程序。
During active exploration programs drillholes are radiometrically logged using calibrated downhole GeoVista NGRS and TGGS (Triple GM) gamma probes which collect continuous readings along the length of the drillhole. Preliminary radiometric equivalent uranium grades ("eU3O8") are then calculated from the downhole radiometric results. The probe is calibrated using an algorithm calculated from the calibration of the probe at the Saskatchewan Research Council facility in Saskatoon and from the comparison of probe results against geochemical analyses. At extremely high radiometric equivalent uranium grades, downhole gamma probes may become saturated, resulting in the probe being overwhelmed, which in turn can create difficulties in accurately determining extremely high-grade radiometric equivalent uranium grades. The equivalent uranium grades are preliminary and are subsequently reported as definitive assay grades following sampling and chemical analysis of the mineralized drill core. In the case where core recovery within a mineralized intersection is poor or non-existent, radiometric grades are considered to be more representative of the mineralized intersection and may be reported in the place of assay grades. Radiometric equivalent probe results are subject to verification procedures by qualified persons employed by CanAlaska prior to disclosure.
在積極的勘探計劃中，使用經過校準的井下GeoVista NGRS和TGGS（Triple GM）伽瑪探測器對鑽孔進行輻射測量，這些探測器沿鑽孔長度收集連續讀數。初步的放射當量鈾等級（“歐盟3O8“）然後根據井下輻射測量結果計算。該探測器是使用一種算法進行校準的，該算法是根據位於薩斯卡通的薩斯喀徹溫研究委員會設施的探測器校準以及探測結果與地球化學分析的比較計算得出的。在極高的輻射當量鈾等級下，井下伽瑪探測器可能會變得飽和，從而導致探測器不堪重負，這反過來又會給準確確定極高等級的輻射當量鈾等級帶來困難。當量的鈾等級是初步的，隨後在對礦化鑽芯進行採樣和化學分析後報告爲最終的化驗等級。如果礦化交叉點內的岩心回收率不佳或不存在，則放射性等級被認爲更能代表礦化交叉點，可以用放射性等級來代替化驗等級。在披露之前，輻射等效探測結果需要經過Canalaska僱用的合格人員的驗證程序。
All reported depths and intervals are drill hole depths and intervals, unless otherwise noted, and do not represent true thicknesses, which have yet to be determined.
除非另有說明，否則所有報告的深度和間隔均爲鑽孔深度和間隔，並不代表尚未確定的真實厚度。
CanAlaska Uranium Ltd. (TSXV: CVV) (OTCQX: CVVUF) (FSE: DH7) holds interests in approximately 500,000 hectares (1,235,000 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 on the West McArthur JV project and Denison on the Moon Lake South JV project 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 .
加拿大阿拉斯卡鈾業有限公司（多倫多證券交易所股票代碼：CVV）（場外交易代碼：CVVUF）（FSE：DH7）持有位於加拿大阿薩巴斯卡盆地（“鈾的沙特阿拉伯”）約50萬公頃（123.5萬英畝）的權益。Canalaska的戰略資產吸引了主要的國際礦業公司。Canalaska目前正在與Cameco合作開展西麥克阿瑟合資項目，與丹尼森合作開展東阿薩巴斯卡盆地的南月湖合資項目。Canalaska是一個項目生成器，有望在世界上最富有的鈾區成功發現。該公司還持有可能開採鎳、銅、金和鑽石的房產。欲了解更多信息，請訪問。
The Qualified Person under National Instrument 43-101 Standards of Disclosure for Mineral Projects for this news release is Nathan Bridge, MSc., P. Geo., Vice-President Exploration for CanAlaska Uranium Ltd., who has reviewed and approved its contents.
本新聞稿符合國家儀器43-101礦產項目披露標準的合格人員是Canalaska鈾業有限公司勘探副總裁Nathan Bridge，理學碩士，P. Geo.，他已經審查並批准了新聞稿的內容。
On behalf of the Board of Directors
"Cory Belyk"
Cory Belyk, P.Geo., FGC
CEO, President and Director
CanAlaska Uranium Ltd.
代表董事會
“Cory Belyk”
Cory Belyk，P.Geo.，FGC
首席執行官、總裁兼董事
Canalaska 鈾有限公司
Cory Belyk, CEO and President
Tel: +1.306.668.6900
Email: cbelyk@canalaska.com
General Enquiry
Tel: +1.306.668.6915
Email: info@canalaska.com
Cory Belyk，首席執行官兼總裁
電話：+1.306.668.6900
電子郵件：cbelyk@canalaska.com
一般查詢
電話：+1.306.668.6915
電子郵件：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.
多倫多證券交易所風險投資交易所及其監管服務提供商（該術語在多倫多證券交易所風險交易所的政策中定義）均不對本新聞稿的充分性或準確性承擔責任。
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.
本新聞稿中包含的所有涉及公司預期、相信或預期將來會或可能發生的活動、事件或發展的陳述均爲前瞻性陳述。這些前瞻性陳述涉及公司根據其經驗、對歷史趨勢的看法、當前狀況、預期的未來發展以及它認爲適合具體情況的其他因素做出的許多假設。此外，這些陳述涉及大量已知和未知的風險和不確定性，這些風險和不確定性加劇了預測、預測、預測和其他前瞻性陳述可能被證明不準確，其中某些是公司無法控制的。讀者不應過分依賴前瞻性陳述。除非法律要求，否則公司無意在本聲明發布之日之後修改或更新這些前瞻性陳述，也無意對其進行修改以反映未來意想不到的事件的發生。
