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WATERFOUND
DRILLING RESULTS
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Sample analyses received from all holes
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New results from hole WF05 encouraging
- Uranium
in holes 700 m apart
Pitchstone
Exploration Ltd. ("Pitchstone") reports additional
encouraging results from the recently completed drilling program
at the Waterfound uranium exploration project in the eastern Athabasca
Basin, Saskatchewan. Analytical results of a total of 202 samples
from all five holes drilled have now been received. The Waterfound
drilling was funded by sxr Uranium One Inc. (TSX: SXR), which
is earning a 50% interest in five of Pitchstone's Athabasca Basin
projects.
A radioactive
zone at the basal Athabasca Group unconformity was encountered in
drill hole WF05. The mineralized 0.5 m core interval is partly in
Athabasca sandstone, partly in underlying graphitic-pyritic metapelites
and averages 202 ppm uranium (0.02 % U3O8). This is about 40 times
the uranium background of basal sandstone, which is typically less
than 5 ppm. Hole WF05 offset hole WF03 by 40 m and these two holes
are on a section 700 m east of WF02 (see
Waterfound map).
As previously
announced, a 2.8 m core interval straddling the unconformity in
hole WF02 averages 94 ppm uranium, including 338 ppm (0.04 % U3O8)
over a 0.39 m interval of sandstone immediately above the unconformity
(News Release 06.05, Dec. 23, 2005). Although a structural control
to the mineralization has not yet been identified, fracturing and
minor faulting are present. Uranium at Waterfound is accompanied
by an enrichment in other metals often encountered in major deposits
in the eastern Athabasca Basin.
Analytical results
have also indicated a significant boron anomaly at Waterfound (to
910 ppm). Increased levels of boron are considered significant as
it is present in the alteration halo at the large, high grade Millennium,
McArthur River and Key Lake deposits in the Athabasca basin.
Drilling at
Waterfound has indicated anomalous mineralization associated with
a six kilometer long conductive zone. Significant features associated
with this zone include:
- Uranium mineralization
at the unconformity to 0.04 % U3O8
- Enrichment
in cobalt, copper, nickel, lead, zinc, arsenic, vanadium and rare
earth elements
- Anomalous
radioactivity associated with lost core above the unconformity
- An alteration
halo that includes chloritization, silicification, dravitization
(boron), hematitization, bleaching and moderate clay alteration
- A thick sequence
of graphite-pyrite-garnet-cordierite pelitic rocks immediately
below the Athabasca Group basal unconformity.
Pitchstone considers
this new uranium mineralized interval in hole WF05 to be very significant
as it has extended the zone at Waterfound. Combined with results
previously reported from drill holes WF02 and WF03, a uraniferous
alteration zone has now been intersected over a strike length of
more than 700 m. Additional drilling is definitely warranted.
Nick Andrade,
P.Eng., P.Geo., is the Qualified Person for the purposes of NI 43-101
with respect to the technical information in this news release.
Mr. Andrade was formerly Chief Geologist at the Cigar
Lake Mine. Sample preparation and analyses were done by SRC Geoanalytical
Laboratories. A partial digestion with chemical analyses (fluorimetry)
was used for uranium determinations.
Pitchstone is
a uranium exploration company with eight exploration projects in
the eastern Athabasca Basin and three in the Hornby Bay Basin, Nunavut
and NWT. These projects include a 50% interest in an inferred uranium
resource in the Mountain Lake deposit, Nunavut (NI 43-101 compliant
estimate; News Release 05.01, Oct. 14, 2005).
For further
information contact:
Ted Trueman, CEO,
(604) 687-3520,
ted@pitchstone.net;
Mark T. Brown,
CFO,
(604) 687-3520,
mtbrown@pacificopportunity.com
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