TSX-V: URC
HIGHLIGHTS:
- New mineralized zone (Joel zone) 2 kilometres southeast of
A4 zone with up to 21 metres of 0.032% U3O8 (316ppm or 0.63 lbs/t)
in surface channeling
- Extensive areas of uranium mineralization encountered on
Pontbriand claims
VANCOUVER,
Dec. 16, 2011 /PRNewswire/ -
Uracan Resources Ltd. (the "Company") (TSX-V: URC) is
pleased to announce the discovery of new areas of significant
uranium mineralization on the Pontbriand and Costebelle claim
groups of its 100% owned North Shore Property in Quebec. This work was part of the summer
2011 exploration program, in the assessment of the airborne
radiometric anomalies and lake sediment anomalies that had not
previously been explored.
Results include 21 metres of 0.032% U3O8 (316
ppm or 0.63 lbs/t) at the Joel Zone (Costebelle C), 17 metres of
0.039% U3O8 (388 ppm or 0.78 lbs/t) at the Pontbriand B South Zone,
12 metres grading 0.038% U3O8 (384 ppm or 0.77 lbs/t) and 5 metres
of 0.030% U3O8 (297ppm or 0.59 lbs/t) at the Pontbriand C Zone, 10
metres grading 0.025% U3O8 (248 ppm or 0.5 lbs/t) at the South JF
Zone (Pontbriand A). All sample results are from surface saw
channel samples.
The mineralized zones on the Pontbriand and
Costebelle claims are generally open in all directions as channel
sampling was limited to areas of existing outcrop exposure, with
shallow overburden cover overlaying large areas of the targeted
airborne anomalies. The main host for uranium mineralization
on the property continues to be granite and granitic pegmatite
intrusive dykes and sills. Please refer to the discussion
below for more details.
Pontbriand Claim Groups
The Pontbriand claim groups (A, B, C and D)
reconnaissance prospecting during 2010 identified a number of new
target areas defined by channel sampling, including 7 metres of
0.128% U3O8 (1275 ppm or 2.56 lbs/t) (Pontbriand B3 Zone), 4 metres
grading 0.115% U3O8 (1153 ppm or 2.31 lbs/t) (Pontbriand A2 Zone)
and 2 metres grading 0.265% U3O8 (2652 ppm or 5.30 lbs/t)
(Pontbriand A2 Zone).
The Pontbriand Claim Group consists of 4
separate areas; Pontbriand A, B, C, and D. The Pontbriand
claims cover a total of approximately 160 square kilometres.
The highway passes through the A and D claim groups, with all the
Pontbriand claims being located within 19 kilometres of the
highway. In addition the main hydro power transmission lines
for the area pass through the claims.
Exploration work completed during 2011 consisted
of mapping, prospecting and channel sampling of the areas initially
discovered in 2010, as well as along strike from the 2010
channels. Additional radiometric anomalies areas were
prospected and mapped throughout the claim group.
The Pontbriand A (southend) zone is a series of
radiometric anomalies occurring along a strike length of
approximately 4.0 kilometres. The South JF zone on the
Pontbriand A claims lies along strike, approximately 1.7 kilometres
northeast of the Pontbriand A (southend) zone, and may represent a
continuation of the mineralized zone seen at the southend
zone. It has a strike length of approximately 0.6 kilometres
as defined by geological mapping, channel sampling and airborne and
ground radiometric surveys. This zone remains open along
strike in both directions.
The Pontbriand B South zone has a strike length
of approximately 1.3 kilometres as defined by geological mapping,
channel sampling and airborne and ground radiometric surveys.
This zone has a northeast trend and remains open along strike.
The Pontbriand C claims cover a domal structure
which hosts 3 mapped and sampled mineralized pegmatite bodies with
strike lengths of 0.8 kilometres, 1.3 kilometres and 2.9 kilometres
on the eastern portion of the claim group. The pegmatite
bodies occur parallel to the metasedimentary bedding in the domal
structure. Additional pegmatite bodies with high radiometric
signatures were mapped but not sampled. Additional follow up
work is required to further define mineralization on the Pontbriand
C claim group.
The Coffin zone has a strike length of
approximately 2.7 kilometres as defined by geological mapping,
channel sampling and airborne and ground radiometric surveys.
The Pontbriand D zone has a strike length of approximately 0.5
kilometres as defined by geological mapping, channel sampling and
airborne and ground radiometric surveys. This zone remains
open along strike.
Pegmatites hosted by metasediments are the main
uranium host on the Pontbriand claims. Geological mapping, channel
sampling and ground radiometric surveys were completed to further
define the mineralized zones on the Pontbriand claims. A map
outlining the various mineralized zones on the Pontbriand claim
group will be available shortly on Uracan's website
www.uracan.ca.
Highlights of the 2011 channel sampling include
17 metres of 0.039% U3O8 (388 ppm or 0.78 lbs/t) at the Pontbriand
B South Zone, 12 metres grading 0.038% U3O8 (384 ppm or 0.77 lbs/t)
and 5 metres of 0.030% U3O8 (297ppm or 0.59 lbs/t) at the
Pontbriand C Zone, 10 metres grading 0.025% U3O8 (248 ppm or 0.5
lbs/t) at the South JF Zone (Pontbriand A), in saw channel
samples. Mineralization is predominantly hosted by granite
and pegmatite dykes intruding metasediments and sedimentary
gneisses.
Selected intervals from the Pontbriand claims
are outlined in the table below:
Claim Group |
Location |
Channel # |
From (m) |
To (m) |
Length (m) |
U3O8 % |
U3O8 ppm |
Pontbriand A |
Pontbriand A zone
(south end) |
CAF11-003 |
0 |
2 |
2 |
0.043 |
432 |
Pontbriand A |
South JF Zone |
CAF11-006 |
2 |
12 |
10 |
0.025 |
248 |
Pontbriand A |
South JF Zone |
CAF11-007 |
0 |
4 |
4 |
0.025 |
246 |
Pontbriand A |
South JF Zone |
CAF11-008 |
0 |
3.5 |
3.5 |
0.024 |
241 |
Pontbriand A |
South JF Zone |
CAF11-010 |
0 |
7 |
7 |
0.041 |
407 |
Pontbriand A |
South JF Zone |
CAF11-011 |
0 |
4 |
4 |
0.020 |
198 |
Pontbriand A |
South JF Zone |
CAF11-012 |
0 |
7 |
7 |
0.020 |
199 |
Pontbriand A |
South JF Zone |
CAF11-013 |
10 |
14 |
4 |
0.045 |
447 |
Pontbriand A |
South JF Zone |
CAF11-
15/016 |
0 |
13 |
13 |
0.030 |
301 |
Pontbriand A |
South JF Zone |
CAF11-017 |
1 |
9 |
8 |
0.024 |
238 |
Pontbriand A |
South JF Zone |
CAF11-018 |
0 |
4 |
4 |
0.019 |
191 |
Pontbriand B |
Pontbriand B
south |
CAF11-027 |
0 |
10 |
10 |
0.021 |
214 |
Pontbriand B |
Pontbriand B
south |
CAF11-028 |
0 |
17 |
17 |
0.039 |
388 |
Pontbriand C |
Pontbriand C Zone |
CAF11-032 |
0 |
12 |
12 |
0.023 |
232 |
Pontbriand C |
Pontbriand C Zone |
CAF11-035 |
0 |
3 |
3 |
0.063 |
625 |
Pontbriand C |
Pontbriand C Zone |
CAF11-036 |
0 |
12 |
12 |
0.038 |
384 |
Pontbriand C |
Pontbriand C Zone |
CAF11-040 |
1 |
6 |
5 |
0.030 |
297 |
Pontbriand C |
Pontbriand C Zone |
CAF11-044 |
1 |
3 |
2 |
0.043 |
432 |
Pontbriand D |
Coffin Zone
(Pontbriand D) |
CAF11-004 |
0 |
3 |
3 |
0.029 |
289 |
Pontbriand D |
Pontbriand D zone |
CAF11-020 |
6 |
8 |
2 |
0.026 |
259 |
Pontbriand D |
Pontbriand D zone |
CAF11-022 |
10 |
11 |
1 |
0.064 |
644 |
Costebelle Claim Group - CC-10 Zone and Joel
Zone
Exploration in the area of the Costebelle A4 and
CC-11 zones has outlined additional drill ready targets within a
few kilometres of the A4 and CC-11 zones. These new target
areas have significantly increased the potential to define a
significant uranium resource hosted in multiple target areas in
close proximity to one another.
The CC-10 Zone is an airborne radiometric
anomaly which had received limited sampling in previous exploration
campaigns. This area was mapped and sampled as part of the
2011 exploration program and consists of an 800 metre by 600 metre
area of multiple stacked west dipping mineralized pegmatites hosted
in metasediments. Mineralization remains open along strike, and the
total width of this zone is not known at this time.
CC-10 is located approximately 3 kilometres east
of the A4 Zone, and 1.5 kilometres north of the CC-11 zone.
These mineralized zones are approximately 68 kilometres east of the
Double S, Middle Zone and TJ resource areas containing a total
indicated resource of 21.5 million tonnes containing 3.11 million
kilograms U3O8 (6.86 million pounds), and a total inferred resource
estimate of 140.65 million tonnes containing 16.826 million
kilograms U308 (37.095 million pounds). Please refer to
September 13, 2011 News Release for
more information.
Selected results from CC-10 are outlined in the
table below:
Claim Group |
Location |
Channel # |
From (m) |
To (m) |
Length (m) |
U3O8 % |
U3O8 ppm |
Costebelle C |
CC10 |
CAF11-051 |
6 |
8 |
2 |
0.036 |
356 |
Costebelle C |
CC10 |
CAF11-052 |
0 |
4 |
4 |
0.019 |
187 |
Costebelle C |
CC10 |
CAF11-057 |
0 |
2 |
2 |
0.023 |
227 |
Prospecting and channel sampling between the A4,
CC-11 and CC-10 zones encountered significant uranium
mineralization in a target area called the Joel Zone after the
exploration technician who initially discovered the
mineralization. Work was focused on ground truthing a number
of smaller airborne radiometric anomalies in this area
approximately 2 kilometres southeast of the A4 zone and 0.6
kilometres northwest of the CC-11 zone.
As a result of the thick overburden cover in
this area, the airborne radiometric response of the mineralized
pegmatites is muted. However ground radiometrics, mapping and
prospecting indicate that a mineralized trend extends over an
approximate 0.8 kilometer strike length in this area. Hand dug
trenches encountered significant amounts of uranophane and other
uranium oxide minerals on surface exposures. The
mineralization is hosted by pegmatite dykes.
Significant results include 2 metres grading
0.247% U3O8 (2470 ppm or 4.94 lbs/t), 21 metres of 0.032% U3O8 (316
ppm or 0.63 lbs/t) and 3 metres grading 0.067% U3O8 (668 ppm or
1.34 lbs/t). All samples are saw cut channel samples. The
width of the overall mineralized pegmatite body is not known at
this time.
Selected intervals from the Joel Zone are
outlined in the table below:
Claim Group |
Location |
Channel # |
From (m) |
To (m) |
Length (m) |
U3O8 % |
U3O8 ppm |
Costebelle C |
Joel Zone |
RIN11-001 |
0 |
3 |
3 |
0.067 |
668 |
Costebelle C |
Joel Zone |
RIN11-002 |
0 |
3 |
3 |
0.022 |
220 |
Costebelle C |
Joel Zone |
RIN11-002 |
12 |
33 |
21 |
0.032 |
316 |
Costebelle C |
Joel Zone |
RIN11-004 |
0 |
1 |
1 |
0.033 |
325 |
Costebelle C |
Joel Zone |
RIN11-004 |
3 |
5 |
2 |
0.247 |
2470 |
Costebelle B Claim Group - New Mineralized
Zone
Previous exploration programs carried out only
limited exploration work on the Costebelle B claim group, located
approximately 20 kilometres northwest of the A4 zone and 55
kilometres northeast of the Double S zone. Mapping and
prospecting with follow up channel sampling has outlined a new zone
(210 Zone) extending over a 400 meter strike length along an
azimuth 210 trend. Due to difficult access conditions field
crews were not able to fully evaluate the claims during the
summer's work program, however further work is being planned which
will include line cutting and multiple landing areas for helicopter
supported exploration.
Significant results include 6 metres of 0.057%
U3O8 (567 ppm or 1.13 lbs/t), 6 metres grading 0.023% U3O8 (234 ppm
or 0.46 lbs/t), and 4 metres grading 0.030% U3O8 (296 ppm or 0.6
lbs/t), in saw channel samples. The width of the overall
mineralized pegmatite body is not known at this time.
Selected intervals from the 210 Zone are
outlined in the table below:
Claim Group |
Location |
Channel # |
From (m) |
To (m) |
Length (m) |
U3O8 % |
U3O8 ppm |
Costebelle B |
210 Zone |
RIN11-006 |
0 |
6 |
6 |
0.057 |
567 |
Costebelle B |
210 Zone |
RIN11-007 |
1 |
7 |
6 |
0.023 |
234 |
Costebelle B |
210 Zone |
RIN11-008 |
1 |
5 |
4 |
0.030 |
296 |
Costebelle B |
210 Zone |
RIN11-009 |
0 |
2 |
2 |
0.019 |
195 |
Costebelle B |
210 Zone |
RIN11-009 |
5 |
14 |
9 |
0.019 |
191 |
Sampling Methodology
Channel samples were collected across areas of
interest marked by geological personnel using rock saws to cut
channels in the bedrock. Channel sample intervals were
generally 1 metre in length. All sample locations were marked
in the field with handheld GPS or Trimble units. The samples
were shipped by Company personnel in sealed containers to ALS
Chemex Laboratories of Val D'Or,
Quebec for analysis using standard analytical techniques for
the samples. ALS Chemex is the laboratory facility used for
all assays from the North Shore Property program.
Uracan Resources Ltd., is a publicly-listed
uranium exploration company, exploring for shallow, bulk
tonnage-style uranium mineralization in Canada. Uracan is led by a team of
proven exploration and mine entrepreneurs and mine-builders.
The information in this news release has been prepared and reviewed
by Marc Simpson, P. Geo., the
Company's Qualified Person under National Instrument 43-101
standards.
Hires New Investor Relations Manager
Uracan Resources Ltd., is pleased to announce
that it has recently hired Ms. Stephanie
Batory, MBA, as the Investor Relations Manager for the
Company. Ms. Batory is a graduate of the Master of Business
Administration program from the University of
New Brunswick, with experience in investment banking,
corporate finance and investor relations.
CAUTIONARY NOTE REGARDING FORWARD-LOOKING
INFORMATION
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. The foregoing information
may contain forward-looking information relating to the future
performance of the Company. Forward looking information is
subject to a number of known and unknown risks, uncertainties and
other factors that may cause actual results to differ materially
from those anticipated in our forward looking
statements. Such risks and other factors
include, among others, the actual results of exploration
activities, changes in world commodity markets or equity markets,
the risks of the mining industry including, without
limitation, those associated with the environment, delays in
obtaining governmental approvals, permits or financing or in the
completion of development or construction activities, title
disputes, change in government and changes to regulations affecting
the mining industry, and other risks and uncertainties detailed
from time to time in the Company's filings with the Canadian
securities administrators (available at www.SEDAR.com
). Forward-looking statements are made based on various
assumptions and on management's beliefs, estimates and opinions on
the date the statements are made. Should one or more of these
risks and uncertainties materialize, or should underlying
assumptions prove incorrect, actual results may vary materially
from those described in the forward-looking information contained
herein. The Company undertakes no obligation to update
forward-looking statements if these assumptions, beliefs, estimates
and opinions or other circumstances should change, except as
required by applicable law.
SOURCE URACAN RESOURCES LTD.