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 钻孔在 U14.9% 处相交 9.6 米3O8 而且 Drillhole WMA082-4 在 9.9% U处相交 14.5 米3O8
Management Attending Investor Clubhouse at the RBC Open June 1, 2024
管理层在2024年6月1日的加拿大皇家银行公开赛上参加投资者俱乐部会所
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.
不列颠哥伦比亚省温哥华--（Newsfile Corp.-2024 年 5 月 29 日）- 加拿大阿拉斯加铀业有限公司（多伦多证券交易所股票代码：CVV） (OTCAX: CVVUF) (FSE: DH7) （“CanAlaska” 或 “公司”）很高兴地报告说，它已经收到了2024年冬季在派克区完成的钻孔的化验结果。地球化学分析结果证实了以 WMA082-6 分级为重点的复合高等级交叉点 14.9%3O8 超过 9.6 米，以及 WMA082-4 分级 上涨9.9％3O8 超过 14.5 米。作为阿萨巴斯卡盆地东部的西麦克阿瑟合资企业项目（“项目”）正在进行的冬季勘探计划的一部分，派克区的钻探已经完成。西麦克阿瑟项目是与Cameco公司的合资企业，由Canalaska运营，该公司持有该项目83.35％的所有权（图1）。Canalaska正在为2024年西麦克阿瑟计划提供独家资金，进一步增加了其在该项目中的多数股权。
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 首席执行官科里·贝利克评论说， “通过化验确认冬季项目在派克区遇到的极高品位铀矿化是评估该项目和合资企业下一步行动的关键步骤。在计划于6月初开始的夏季钻探计划中，Canalaska团队将重点扩大已知的不合格相关高品位铀区域。我们仍然相信，派克区是潜在的一级矿化事件，这是基于在不整合处相交的铀的经过验证的等级和厚度、相关的深层基底矿化根系，以及在派克区和目标走廊沿线其他地方观察到的岩心结构和蚀变特征。基于阿萨巴斯卡盆地东部其他高品位铀矿床类似物，例如麦克阿瑟河，派克区可能只是几颗珍珠中的一颗。”
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.
该公司很高兴地宣布，西麦克阿瑟项目的2024年冬季钻探计划已经完成。2024年冬季计划的重点是继续扩大派克区的发现范围，并将罢工不合格测试扩展到派克区的东北和西南部。在钻探计划中，共完成了八项不合格目标测试，总长度为6,201米。在派克区完成的所有三个钻孔（WMA082-4、WMA082-5、WMA082-6）都与铀矿化区相交。WMA082-4 和 WMA082-6 钻孔中的矿化是迄今为止在西麦克阿瑟项目上钻探的最高品位的矿化交叉点。
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).
地球化学分析结果证实，WMA082-4 钻孔与一个 7.4% 的铀的主要复合间隔相交3O8 超过 19.5 米，包括 9.9%3O8 超过 14.5 米，随后在井下还有几个额外的矿化间隔（表 1）。WMA082-4 中的矿化特征是块状到半块状、气泡状、弥漫性、粘土状和裂缝控制的铀矿化，与阿萨巴斯卡砂岩与底层基底岩接触处的黄色和橙色二级铀有关。矿化间隔位于粘土和亚氯酸盐强烈蚀变的广阔区域内，从而完全取代了原有的岩石结构和纹理。由于地质条件不佳，没有岩心回收的间隔在 WMA082-4 矿化交叉点内相交。在没有岩心回收的间隔内，根据更新的辐射等效品位曲线计算得出的井下辐射当量铀等效品位曲线，该曲线与冬季钻探计划期间获得的地球化学分析结果相关，被插入缺失岩心并作为更大综合间隔的一部分进行报告（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).
地球化学分析结果证实，WMA082-6 钻孔与一个 12.9% 的铀的主要复合间隔相交3O8 超过 11.1 米，包括 14.9% 的铀3O8 超过 9.6 米，随后在井下还有一个额外的矿化间隔（表 2）。WMA082-6 中的矿化直接存在于阿萨巴斯卡砂岩与下层基底岩石之间的不整合接触处，其特征是与黄色和橙色铀次级矿化以及赤铁矿蚀变相关的块状到半块状铀矿化。铀矿化延伸到 WMA082-6 的基底岩石中，其特征是铀矿化的结核状、浸染、粘土托管、叶片控制和裂缝控制的矿脉，与局部的淡黄色铀次生矿和强烈的基底变化有关。在 WMA082-6 矿化交叉点内有一段没有岩心回收的间隔。在这段没有岩心回收的间隔内，根据更新的辐射等效品位曲线计算得出的井下辐射当量铀等效品位曲线，该曲线与冬季钻探计划期间获得的地球化学分析结果相关，被插入缺失岩心并作为更大综合间隔的一部分进行报告（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).
地球化学分析结果证实，WMA082-5 钻孔与一个间隔的砂岩托管铀矿化区相交，铀矿化等级为 1.5%3O8 超过 4.6 米（表 3）。WMA082-5 中的矿化位于阿萨巴斯卡砂岩与底层岩石之间的不整合接触点正上方。WMA082-5 中的矿化特征是浸染铀和结核铀矿化位于深灰色至黑色硫化物和粘土变化的砂岩柱中，由于岩石脆性高，岩石易碎性高，岩心会出现局部丢失间隔。不合格之处正下方的 WMA082-5 基底被强烈的粘土和亚氯酸盐改变，导致原来的岩石织物纹理被取代。在 WMA082-5 矿化交叉点内有一段没有岩心回收的间隔。在这段没有岩心回收的间隔内，根据更新的辐射等效品位曲线计算得出的井下辐射当量铀等效品位曲线，该曲线与冬季钻探计划期间获得的地球化学分析结果相关，被插入缺失岩心并作为更大综合间隔的一部分进行报告（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).
派克区的最新钻探围栏位于与 WMA082-2 相交的高品位铀矿化区走向东北约 30 米处，该矿化区与 1.03% 的铀相交3O8 超过 6.3 米，包括 2.82% U 的子间隔3O8 超过 1.9 米（参见 2024 年 1 月 18 日的新闻稿）。目前，派克区的不合格目标在 WMA082-4、WMA082-5 和 WMA082-6 周围的各个方向上仍然是开放的（图 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.
该公司正在积极规划西麦克阿瑟项目的2024年夏季演习计划。钻探计划预计将于6月初开始，将包括两台金刚石钻机，目标是再钻探约9,000米。该计划预计将于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，该公司还保留了萨斯卡通明德矿产资源有限公司（“Underseded”）的服务。在Understeed的协助下，该公司利用经地球化学分析确认的来自派克区的交叉点，生成了更新的辐射探测器等效等级曲线。这条更新的辐射探测器当量曲线考虑了冬季钻探计划期间相交的超高等级探测器等效曲线，将允许对未来潜在的高品位交叉点进行更明确的当量铀计算。Unfersed还将为公司提供基于地统计学的资源建模服务，为未来可能在派克区进行资源计算做准备。
Table 1 - WMA082-4 Intersections with Geochemical Assay and Radiometric Equivalent Intervals
表 1-含地球化学分析和辐射等效间隔的 WMA082-4 交叉点
|
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 间隔 1
|
来自
(m)
|
到
(m)
|
长度
(m)7
|
平均成绩
|
|
(% U)3O8)
|
(% 欧盟3O8)8
|
| 间隔 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 |
|
|
复合间隔 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 |
|
| |
|
|
|
|
|
| 间隔 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 |
|
| |
|
|
|
|
|
| 间隔 3 (6)
|
829.6 |
831.6 |
2.0 |
0.4 |
|
- WMA082-4 钻探的方位角为 295，倾角为 -79.3，钻孔为 477,345 mE/6,396,525 mN，A.S.L. 605 米（UTM NAD83 Z13N）。
- 交叉间隔在截止等级高于 0.1% U 时合成3O8 /欧盟3O8 最大内部稀释量为 1.0 m。
- 复合间隔包含回收岩心的地球化学分析，并插入井下辐射等效铀等效等效品位来代替缺失的岩心间隔。
- 交叉间隔的合成比例高于 1.0% U 的截止等级3O8 最大内部稀释量为 1.0 m。
- 交叉间隔的合成比例高于 1.0% U 的截止等级3O8 /欧盟3O8 最大内部稀释量为 1.0 m。
- 交叉间隔在截止等级高于 0.1% U 时合成3O8 最大内部稀释量为 1.0 m。
- 除非另有说明，否则所有报告的深度和间隔均为钻孔深度和间隔，并不代表尚未确定的真实厚度。
- 辐射当量（“eU”3O8“) 源自经过校准的井下伽玛探测器。在这些间隔内没有发现任何岩心，用井下辐射等效铀等级来代替缺失的岩心间隔。
|
Table 2 - WMA082-6 Intersections with Geochemical Assay and Radiometric Equivalent Intervals
表 2-含地球化学分析和辐射等效间隔的 WMA082-6 交叉点
|
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 间隔 1
|
来自
(m)
|
到
(m)
|
长度
(m)6
|
平均成绩
|
|
(% U)3O8)
|
(% 欧盟3O8)7
|
| 间隔 1 (2)
|
798.0 |
800.5 |
2.5 |
|
16.7 |
| 800.5 |
809.1 |
8.6 |
11.9 |
|
|
复合间隔 1 (2,3)
|
798.0 |
809.1 |
11.1 |
12.9 |
|
|
包括 (4)
|
798.9 |
808.5 |
9.6 |
14.9 |
|
| |
|
|
|
|
|
| 间隔 2 (5)
|
815.9 |
816.6 |
0.7 |
0.7 |
|
- WMA082-6 钻探的方位角为 295，倾角为 -79.3，钻孔为 477,345 mE/6,396,525 mN，A.S.L. 605 米（UTM NAD83 Z13N）。
- 交叉间隔在截止等级高于 0.1% U 时合成3O8 /欧盟3O8 最大内部稀释量为 1.0 m。
- 复合间隔包含回收岩心的地球化学分析，并插入井下辐射等效铀等效等效品位来代替缺失的岩心间隔。
- 交叉间隔的合成比例高于 1.0% U 的截止等级3O8 /欧盟3O8 最大内部稀释量为 1.0 m。
- 交叉间隔在截止等级高于 0.1% U 时合成3O8 最大内部稀释量为 1.0 m。
- 除非另有说明，否则所有报告的深度和间隔均为钻孔深度和间隔，并不代表尚未确定的真实厚度。
- 辐射当量（“eU”3O8“) 源自经过校准的井下伽玛探测器。在这些间隔内没有发现任何岩心，用井下辐射等效铀等级来代替缺失的岩心间隔。
|
Table 3 - WMA082-5 Intersections with Geochemical Assay and Radiometric Equivalent Intervals
表 3-含地球化学分析和辐射等效间隔的 WMA082-5 交叉点
|
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 间隔 1
|
来自
(m)
|
到
(m)
|
长度
(m)5
|
平均成绩
|
|
(% U)3O8)
|
(% 欧盟3O8)6
|
| 间隔 1 (2)
|
804.3 |
805.0 |
0.7 |
|
0.15 |
| 805.0 |
808.9 |
3.9 |
1.7 |
|
|
复合间隔 1 (2,3)
|
804.3 |
808.9 |
4.6 |
1.5 |
|
|
包括 (4)
|
806.4 |
808.4 |
2.0 |
3.2 |
|
- WMA082-5 钻探的方位角为 295，倾角为 -79.3，钻孔为 477,345 mE/6,396,525 mN，A.S.L. 605 米（UTM NAD83 Z13N）。
- 交叉间隔在截止等级高于 0.1% U 时合成3O8 /欧盟3O8 最大内部稀释量为 1.0 m。
- 复合间隔包含回收岩心的地球化学分析，并插入井下辐射等效铀等效等效品位来代替缺失的岩心间隔。
- 交叉间隔的合成比例高于 1.0% U 的截止等级3O8 最大内部稀释量为 1.0 m。
- 除非另有说明，否则所有报告的深度和间隔均为钻孔深度和间隔，并不代表尚未确定的真实厚度。
- 辐射当量（“eU”3O8“) 源自经过校准的井下伽玛探测器。在这些间隔内没有发现任何岩心，用井下辐射等效铀等级来代替缺失的岩心间隔。
|
The Company will have management representatives at the Investor Clubhouse at the RBC Open on June 1, 2024 in Hamilton, Ontario.
公司将于2024年6月1日在安大略省汉密尔顿举行的加拿大皇家银行公开赛的投资者俱乐部派出管理层代表。
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 年计划中的所有钻芯样本均运送到位于萨斯喀彻温省萨斯卡通的萨斯喀彻温省研究委员会地质分析实验室 (SRC)，采用总量 (Hf: nho3: HCL) 和部分消化 (HnO3: HCL)、聚变硼和铀进行制备、处理和多元素分析，由 ICP-MS 和 ICP-OES 进行制备、处理和多元素分析3O8 ICP-OES 使用更高级别的标准对 wt% 进行测定。化验样本是根据井下探测的辐射等效铀等级和闪烁计（SPP2 或 CT007-M）峰值来选择的。化验样本间隔包括矿化间隔内 0.3-0.8 米的连续半核分裂样品。选择的密度样本，包括0.1米连续的整个岩心样本，随后进行分割和分析，可以在矿化间隔内采集。对于所有化验样本，保留一半的拆分样本，另一半发送到SRC进行分析。SRC 是经过 ISO/IEC 17025/2005 和加拿大标准委员会认证的分析实验室。根据Canalaska的质量保证/质量控制（QA/QC）程序，CanAlaska和SRC定期将空白、标准参考材料和重复样本插入样本流。在披露之前，地球化学分析数据必须经过Canalaska雇用的合格人员的验证程序。
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.
在积极的勘探计划中，使用经过校准的井下GeoVista NGRS和TGGS（Triple GM）伽玛探测器对钻孔进行辐射测量，这些探测器沿钻孔长度收集连续读数。初步的放射当量铀等级（“欧盟3O8“）然后根据井下辐射测量结果计算。该探测器是使用一种算法进行校准的，该算法是根据位于萨斯卡通的萨斯喀彻温研究委员会设施的探测器校准以及探测结果与地球化学分析的比较计算得出的。在极高的辐射当量铀等级下，井下伽玛探测器可能会变得饱和，从而导致探测器不堪重负，这反过来又会给准确确定极高等级的辐射当量铀等级带来困难。当量的铀等级是初步的，随后在对矿化钻芯进行采样和化学分析后报告为最终的化验等级。如果矿化交叉点内的岩心回收率不佳或不存在，则放射性等级被认为更能代表矿化交叉点，可以用放射性等级来代替化验等级。在披露之前，辐射等效探测结果需要经过Canalaska雇用的合格人员的验证程序。
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.
除非另有说明，否则所有报告的深度和间隔均为钻孔深度和间隔，并不代表尚未确定的真实厚度。
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 .
加拿大阿拉斯卡铀业有限公司（多伦多证券交易所股票代码：CVV）（场外交易代码：CVVUF）（FSE：DH7）持有位于加拿大阿萨巴斯卡盆地（“铀的沙特阿拉伯”）约50万公顷（123.5万英亩）的权益。Canalaska的战略资产吸引了主要的国际矿业公司。Canalaska目前正在与Cameco合作开展西麦克阿瑟合资项目，与丹尼森合作开展东阿萨巴斯卡盆地的南月湖合资项目。Canalaska是一个项目生成器，有望在世界上最富有的铀区成功发现。该公司还持有可能开采镍、铜、金和钻石的房产。欲了解更多信息，请访问。
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.
本新闻稿符合国家仪器43-101矿产项目披露标准的合格人员是Canalaska铀业有限公司勘探副总裁Nathan Bridge，理学硕士，P. Geo.，他已经审查并批准了新闻稿的内容。
On behalf of the Board of Directors
"Cory Belyk"
Cory Belyk, P.Geo., FGC
CEO, President and Director
CanAlaska Uranium Ltd.
代表董事会
“Cory Belyk”
Cory Belyk，P.Geo.，FGC
首席执行官、总裁兼董事
Canalaska 铀有限公司
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，首席执行官兼总裁
电话：+1.306.668.6900
电子邮件：cbelyk@canalaska.com
一般查询
电话：+1.306.668.6915
电子邮件：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.
多伦多证券交易所风险投资交易所及其监管服务提供商（该术语在多伦多证券交易所风险交易所的政策中定义）均不对本新闻稿的充分性或准确性承担责任。
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.
本新闻稿中包含的所有涉及公司预期、相信或预期将来会或可能发生的活动、事件或发展的陈述均为前瞻性陈述。这些前瞻性陈述涉及公司根据其经验、对历史趋势的看法、当前状况、预期的未来发展以及它认为适合具体情况的其他因素做出的许多假设。此外，这些陈述涉及大量已知和未知的风险和不确定性，这些风险和不确定性加剧了预测、预测、预测和其他前瞻性陈述可能被证明不准确，其中某些是公司无法控制的。读者不应过分依赖前瞻性陈述。除非法律要求，否则公司无意在本声明发布之日之后修改或更新这些前瞻性陈述，也无意对其进行修改以反映未来意想不到的事件的发生。
