CanAlaska Uranium Ltd. - Uranium-gold-platinum mineralization found at Poplar project, northern Athabasca Basin



    VANCOUVER, Feb. 6 /CNW/ - CanAlaska Uranium Ltd. (TSX.V - CVV)
("CanAlaska" or the "Company") is pleased to announce results from summer
prospecting on its Poplar project. Multiple zones of uranium mineralization
were detailed in basement rocks, just north of the northern limit of the
Athabasca sandstone. High gold and platinum values are associated with two of
the showings. The Poplar project straddles 120 km of the northern edge of the
Athabasca Basin in Northern Saskatchewan.

    Poplar Project Location

    http://www.canalaska.com/i/maps/PPL2009-02-03Figure1-Location.pdf

    In 2008, CanAlaska survey crews completed over 15,000 line-kms of shallow
seismic profiling over the northern portion of Lake Athabasca, detailing the
edge of the Athabasca sandstone, and the features surrounding numerous
airborne conductors discovered by the previous season's airborne (VTEM)
geophysical surveys.

    http://www.canalaska.com/i/maps/PPL2009-02-03Figure2-Prospecting.pdf

    Prospecting during summer 2008 included work on 13 new and historical
uranium showings located along the north shore of Lake Athabasca. These
showings are hosted in various rocks of the Murmac Bay Group and a series of
granites. The assay results for the samples collected from these zones are
reported below.
    There are three significant areas of mineralized showings (See Figure 2).
Within these areas, two types of mineralizing styles are recognised:

    
    1.  Metamorphic re-concentrations in pegmatitic to granitic rocks with a
        low U/Th ratio; these showings contain less than 1 % U(3)O(8).
    2.  Hydrothermal vein-type showings in a variety of rocks with a high
        U/Th ratio; these showings contain distinctly higher U(3)O(8),
        reaching over 50% U(3)O(8).
    

    The Felix Bay, Sharp Bay, Adair Bay, McIntosh Bay, and Natukam Peninsula
target areas are all in the second, higher-grade mineralized group.
Additionally, significant rare earth mineralization was observed at Adair Bay
in granites/pegmatites associated with the showing (see map).
    The gamma spectrometry survey conducted over the central land portion of
the Poplar Project shows a high total count and high uranium background over
most of the area. This high overall uranium signature, together with the two
types of mineralization, form good precursors for unconformity uranium
deposits in areas of the project to the south.
    The 2008 airborne EM and waterborne seismic surveys which covered the
southern portion of the Poplar project defined a large number of structural
events and zones of high conductivity and disruption in the sandstone cover.
The data from these surveys is currently being compiled by CanAlaska
personnel. There is strong evidence of structural dislocation of these
conductors, especially in the area of the Felix Bay uranium-gold-platinum
mineralization (see Figure 3). The water-covered areas were planned to be
drill-tested this winter season, but with the December termination of the
previous option agreement with Mega Uranium, these targets will be
re-evaluated and re-scheduled for the 2010 season.
    The presence of graphitic conductors in the meta-sedimentary package, as
revealed by the VTEM surveys, and the presence of large scale structural
disturbances, combine well with the uranium enriched-basement to enhance the
potential for unconformity uranium deposits on this project.

    Felix Bay Geology

    The most significant samples of multi-element mineralization, including
gold and platinum, are located within a zone of hydrothermal alteration at
Felix Bay in the centre of the exploration area.

    www.canalaska.com/i/maps/PPL2009-02-03Figure3-FelixBayArea.pdf

    At this location, a N-S trending sulphidic pelite is mineralized by E-W
trending veinlets of pitchblende uranium mineralization, accompanied by
chloritic and sericite alteration. One grab sample from very old blast pits
assayed 46.9 g/t gold and 19.7 g/t platinum and 20.8g/t palladium. The
mineralization is visible over 10 x 50 metres along the shoreline of the bay.
It appears to be parallel to, or be associated with, a mapped iron formation
unit.
    A N-S trending EM conductor (see Figure 3) follows the bay and is offset
300 metres inland near the showing. Very limited historical drilling during
the 1950's did not report uranium mineralization at depth at the showings near
the lake, but several drill-holes were lost in bad ground and did not approach
the target. The original samples appear to have only been assayed for uranium.
Old reports predicted the expansion of the target further to the south, where
a large NE-SE structure is predicted to intercept the horizon.

    
    Table 1 Felix Bay Zone - Blast Pit samples
    -------------------------------------------------------------------------
    Sample        % U3O8        Au g/t       Pt g/t       Pd g/t        U/Th
    -------------------------------------------------------------------------
    DT091          10.24         1.14         0.33         0.43        363.7
    -------------------------------------------------------------------------
    DT093           4.27        46.94         19.7        20.83        439.7
    -------------------------------------------------------------------------
    MG077            1.2         0.05          N/A          N/A          265
    -------------------------------------------------------------------------
    MG074           0.06            0          N/A          N/A          2.8
    -------------------------------------------------------------------------
    MG078           0.05         0.44          N/A          N/A         33.2
    -------------------------------------------------------------------------

    At Sharp Bay, mineralization occurs as pitchblende fracture filling in
strongly hematized granites and in strongly hematized amphibolite. The granite
hosted mineralization from the historical "Ingrid" uranium showing exhibits
the higher grade. The amphibolite samples are from outcrop and boulders 0.75
km SW of this showing.

    Table 2 Sharp Bay Grab samples
    -------------------------------------------------------------------------
    Sample  % U3O8       Au g/t          Pt g/t          Pd g/t        U/Th
    -------------------------------------------------------------------------
    CH200    18.87               1   less than 0.1   less than 0.1    1391.3
    -------------------------------------------------------------------------
    JL007     4.12             0.1   less than 0.1   less than 0.1    1203.4
    -------------------------------------------------------------------------
    CH203     0.55             N/A             N/A             N/A     665.7
    -------------------------------------------------------------------------
    CH204     0.33   less than 0.1   less than 0.1   less than 0.1     468.3
    -------------------------------------------------------------------------
    CH201     0.31   less than 0.1   less than 0.1   less than 0.1     323.8
    -------------------------------------------------------------------------
    FT033     0.24   less than 0.1   less than 0.1   less than 0.1     227.8
    -------------------------------------------------------------------------
    CH202     0.18   less than 0.1   less than 0.1   less than 0.1       306
    -------------------------------------------------------------------------
    FT034     0.13   less than 0.1   less than 0.1   less than 0.1     183.3
    -------------------------------------------------------------------------

    At McIntosh Bay, a 2 cm mineralised vein cuts across pelitic rocks, part
of a pelite-quartzite-pegmatite assemblage. The vein can be followed for 40
metres before disappearing in overburden. One sample has high gold values
(34g/t). The neighbouring pegmatites are radioactive and stained yellow.

    Table 3 McIntosh Bay Narrow vein samples
    -------------------------------------------------------------------------
    Sample        % U3O8        Au g/t       Pt g/t       Pd g/t        U/Th
    -------------------------------------------------------------------------
    RD317           3.58         0.29          N/A          N/A        500.1
    -------------------------------------------------------------------------
    GS051           1.42         0.09          N/A          N/A        315.0
    -------------------------------------------------------------------------
    GS053           1.21         0.01          N/A          N/A        388.4
    -------------------------------------------------------------------------
    RCD012          0.79         0.01          N/A          N/A        307.8
    -------------------------------------------------------------------------
    JR457           0.74         34.3          N/A          N/A        377.5
    -------------------------------------------------------------------------
    GS052           0.61         0.06          N/A          N/A        244.0
    -------------------------------------------------------------------------
    GK042           0.32          5.9          N/A          N/A         98.6
    -------------------------------------------------------------------------

    At Natukam Peninsula (Fall Zone), two mineralized veins are associated
with, and parallel to, a trending NW-SE fault, cutting across a NE trending
paragneiss. Several samples are high in gold, with a maximum of 12.4 g/t. The
very high grade uranium samples (up to 58% U(3)O(8)) listed in Table 4 are
small selective samples from the old trenches, representing traces of lower
temperature remobilized pitchblende mineralization along shears and fractures.

    Table 4 Natukum stringer pitchblende uranium grab samples
    -------------------------------------------------------------------------
    Sample  % U3O8       Au g/t          Pt g/t          Pd g/t        U/Th
    -------------------------------------------------------------------------
    CH212    58.25             N/A             N/A             N/A     857.6
    -------------------------------------------------------------------------
    CH217    51.53             N/A             N/A             N/A     906.6
    -------------------------------------------------------------------------
    CH211    45.40             N/A             N/A             N/A     793.8
    -------------------------------------------------------------------------
    CH213    45.40             N/A             N/A             N/A     863.2
    -------------------------------------------------------------------------
    CH214    32.08             N/A             N/A             N/A     944.4
    -------------------------------------------------------------------------
    MG113    23.23             1.5             2.5             2.5    1551.2
    -------------------------------------------------------------------------
    CH216     8.84             N/A             N/A             N/A    1153.8
    -------------------------------------------------------------------------
    CH215     4.14             N/A             N/A             N/A       975
    -------------------------------------------------------------------------
    MG115      3.8            12.4             2.3             3.7     298.1
    -------------------------------------------------------------------------
    MG112     3.05             0.5             0.5             0.5     959.3
    -------------------------------------------------------------------------
    MG118     2.91             0.4   less than 0.1   less than 0.1     333.8
    -------------------------------------------------------------------------
    CH209      2.7             N/A             N/A             N/A     817.9
    -------------------------------------------------------------------------
    MG111     1.79             0.3   less than 0.1   less than 0.1    1013.3
    -------------------------------------------------------------------------
    MG110     1.63   less than 0.1   less than 0.1   less than 0.1       575
    -------------------------------------------------------------------------
    CH210     1.58             N/A             N/A             N/A     837.5
    -------------------------------------------------------------------------

    At Adair Bay, the mineralization occurs as veinlets of pitchblende in
mafic metapelites. Rare Earth-yttrium mineralization is also present,
associated with granitic-pegmatitic rocks with grades ranging from 0.5-2.7%
total REE.

    Table 5 Adair Bay grab samples
    -------------------------------------------------------------------------
    Sample  % U3O8       Au g/t          Pt g/t          Pd g/t        U/Th
    -------------------------------------------------------------------------
    FT057     5.31             3.8             1.5             0.8     661.8
    -------------------------------------------------------------------------
    FT056     4.01             0.1   less than 0.1   less than 0.1     515.2
    -------------------------------------------------------------------------
    AM206     2.57             0.6   less than 0.1   less than 0.1     411.3
    -------------------------------------------------------------------------
    AM207     0.96             N/A             N/A             N/A     337.5
    -------------------------------------------------------------------------
    FT049     0.10   less than 0.1   less than 0.1   less than 0.1         3
    -------------------------------------------------------------------------

    The Hill Lake showing, shown in Figure 4, consists of a three kilometre
long zone within a strongly anomalous meta-arkose with patches of white to
pink pegmatite enriched in uranium. The uranium mineralization is mostly in
the biotite enriched phases of these pegmatites.

    Table 6 Hill Lake Zone grab samples
    -----------------------------------------------
    Sample      % U3O8         Au g/t         U/Th
    -----------------------------------------------
    MG131        0.66      less than 0.1       5.1
    -----------------------------------------------
    DTM017       0.43      less than 0.1       8.9
    -----------------------------------------------
    MG132        0.38      less than 0.1       2.2
    -----------------------------------------------
    CM143        0.34      less than 0.1       8.4
    -----------------------------------------------
    RD313        0.25      less than 0.1       2.6
    -----------------------------------------------
    DTM018       0.24      less than 0.1       4.8
    -----------------------------------------------
    CM132        0.20      less than 0.1       9.3
    -----------------------------------------------
    CH233        0.14      less than 0.1      11.3
    -----------------------------------------------
    CM140        0.12      less than 0.1       2.0
    -----------------------------------------------
    CM145        0.12      less than 0.1      11.1
    -----------------------------------------------
    RD333        0.12      less than 0.1       0.6
    -----------------------------------------------
    CM141        0.11                1.7       1.8
    -----------------------------------------------
    DT106        0.11      less than 0.1       4.9
    -----------------------------------------------
    

    http://www.canalaska.com/i/maps/PPL2009-02-03Figure4-HillLakeArea.pdf

    All of the samples from the Poplar project were submitted to Acme
Laboratories Vancouver, an ISO 9001:2000 accredited and qualified Canadian
laboratory, for the Group 4B analysis. These samples were analyzed for uranium
and multi-element geochemistry by tri-acid digestion and ICP-MS. High grade
uranium samples were assayed by Saskatchewan Research Laboratories and
analyzed for multi-element geochemistry, including uranium and other elements
by tri-acid digestion and ICP. Gold, platinum and palladium with significant
gold were analyzed by fire assay. The samples were collected by CanAlaska
field geologists under the supervision of Dr. Karl Schimann, and were shipped
in secure containment to the qualified Canadian laboratories noted above.
    Peter Dasler, M.Sc, P. Geo. is the Qualified Person for this news
release.

    About CanAlaska Uranium Ltd. - www.canalaska.com

    CANALASKA URANIUM LTD. (CVV - TSX.V, CVVUF - OTCBB, DH7 - Frankfurt) is
undertaking uranium exploration in twenty 100%-owned and two optioned uranium
projects in Canada's Athabasca Basin. Since September 2004, the Company has
aggressively acquired one of the largest land positions in the region,
comprising over 2,500,000 acres (10,117 sq. km or 3,906 sq. miles). To-date,
CanAlaska has expended over Cdn$45 million exploring its properties and has
delineated multiple uranium targets. The Company's geological expertise and
high exploration profile has attracted the attention of major international
strategic partners. Among others, Mitsubishi Development Pty., a subsidiary of
Japanese conglomerate Mitsubishi Corporation, has undertaken to provide
CanAlaska C$11 mil. in exploration funding for its West McArthur Project.
Exploration of CanAlaska's Cree East Project is also progressing under a C$19
mil. joint venture with a consortium of Korean companies led by Hanwha
Corporation, and comprising Korea Electric Power Corp., Korea Resources Corp.
and SK Energy Co, Ltd. A Memorandum of Understanding has also recently been
executed with mining partner East Resources Inc. to commence exploration on
the NE Wollaston Project comprising a potential 100,000 metres of drill
testing.

    
    On behalf of the Board of Directors

    (signed)

    Peter Dasler, M.Sc., P.Geo.
    President & CEO, CanAlaska Uranium Ltd.
    


    The TSX Venture has not reviewed and does not accept responsibility for
the adequacy or accuracy of this release: CUSIP No. 13708P 10 2. This news
release contains certain "Forward-Looking Statements" within the meaning of
Section 21E of the United States Securities Exchange Act of 1934, as amended.
All statements, other than statements of historical fact, included herein are
forward-looking statements that involve various risks and uncertainties. There
can be no assurance that such statements will prove to be accurate, and actual
results and future events could differ materially from those anticipated in
such statements. Important factors that could cause actual results to differ
materially from the Company's expectations are disclosed in the Company's
documents filed from time to time with the British Columbia Securities
Commission and the United States Securities & Exchange Commission.





For further information:

For further information: Emil Fung, Vice President, Corp. Dev., Tel:
(604) 688-3211, Email: info@canalaska.com

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