UEX Reports Results of Summer 2009 Exploration on the Hidden Bay Project:
SP-203 Intersects 1.527% U(3)O(8) Over 1.5 Metres at Telephone Lake.
UEX Plans
Trading Symbol: UEX-TSX
"Hidden Bay hosts one of the most significant uranium resources in the Athabasca Basin due primarily to our successful drilling programs in recent years at the Horseshoe and Raven Deposits," said
Results from the Hidden Bay Summer 2009 Drilling Program
The summer 2009 drilling program at Hidden Bay was comprised of 49 drill holes totaling 15,071 metres. Significant mineralization was found in several holes. The program was completed in
- Horseshoe and Raven - designed to test targets peripheral to the Horseshoe and Raven Deposits for possible extensions of mineralization and to assess nearby geophysical and geological targets; - Telephone Lake - designed to follow up previous drilling results and to further explore the Telephone Lake trend. This trend is a major fault zone which contains previous mineralized drill intercepts and extends northward into the Sue Deposits on the adjacent McClean Lake Mine property, operated by AREVA Resources Canada Inc. ("AREVA"); and - Vixen Lake South - designed to test a geophysical anomaly coincident with intense clay alteration in historical drill holes.
Maps of the 2009 drilling at Hidden Bay are available for viewing in the "News Releases" section of UEX's website at www.uex-corporation.com.
Drilling in the Area of the Horseshoe and Raven Deposits
During the winter of 2009, UEX successfully expanded the Horseshoe and Raven Deposits through a stepout drilling program. In
- At a cut-off grade of 0.05% U(3)O(8) total resources are: ------------------------------------------------------------------------- Category Tonnes U(3)O(8)(%) U(3)O(8)(lbs) ------------------------------------------------------------------------- Indicated 10,293,600 0.155 35,044,000 Inferred 1,109,200 0.111 2,715,000 ------------------------------------------------------------------------- - At a lower cut-off grade of 0.02% U(3)O(8) total resources are: ------------------------------------------------------------------------- Category Tonnes U(3)O(8)(%) U(3)O(8)(lbs) ------------------------------------------------------------------------- Indicated 16,688,500 0.108 39,971,000 Inferred 1,982,500 0.079 3,470,000 -------------------------------------------------------------------------
During the summer of 2009, 23 drill holes totaling 7,103 metres were completed in the Horseshoe, Raven and adjacent areas. Thirteen of these holes tested possible extensions of some mineralized zones to assess the potential for resource expansion and for down dip continuation of mineralization. Results of principal intercepts in the Horseshoe and Raven area are reported in Table 1. Drilling intercepts with a grade-thickness product of greater than 0.05 and grades of greater than 0.05% U(3)O(8) include the following:
- 0.076% U(3)O(8) over 4.0 metres, and 0.140% U(3)O(8) over 2.1 metres in hole HU-361 (Horseshoe northeast); - 0.087% U(3)O(8) over 1.0 metre in hole RU-219 (pod on south side of Raven); - 0.107% U(3)O(8) over 4.4 metres in hole RU-225 (Raven west); and - 0.120% U(3)O(8) over 4.6 metres in hole RU-226 (Raven west).
These intercepts slightly expand the strike length of the mineralized zones and would result in a small increase in estimated resources. Other drill holes bounded mineralization down dip.
The remaining drill holes tested geophysical, structural and known alteration targets within one kilometre of the Horseshoe and Raven Deposits. While none of these holes intersected any significant mineralization, areas of intense alteration which could potentially host mineralization were intersected, identifying future targets. Notably, in one deep hole (HU-363) which tested the Dragon Lake Fault on the east side of the Horseshoe Deposit, extensive and intense alteration extends downward for at least 600 metres into basement rocks, forming a potential feeder zone for mineralization. Given the intensity of alteration along this corridor, future drilling will target areas to the south where the Dragon Lake Fault intersects graphitic gneiss.
Telephone Lake
During the summer of 2009, 7,968 metres of drilling in 26 drill holes distributed over a four-kilometre strike length were completed in the Telephone Lake area ("Telephone"). Telephone is located immediately south of the Sue and McClean Lake Deposits and has the potential for the discovery of Sue C, D and E or Eagle Point style basement-hosted mineralization along the Telephone Lake Fault, or where fault systems intersect the sub-Athabasca unconformity.
Drilling in 2009 targeted areas of known mineralization near the unconformity that included previous intercepts of 0.20% U(3)O(8) over 6.8 metres in 2006 drill hole SP-166 and 4.52% U(3)O(8) over 0.5 metres in 2005 drill hole SP-156.
Results of principal intercepts obtained during 2009 at Telephone are reported in Table 1. Drilling intercepts with a grade-thickness product of greater than 0.05 and grades of greater than 0.05% U(3)O(8) include the following:
- 0.110% U(3)O(8) over 0.5 metres in hole SP-191; - 0.100% U(3)O(8) over 2.0 metres, and 0.401% U(3)O(8) over 1.9 metres in hole SP-193; - 0.277% U(3)O(8) over 0.3 metres in hole SP-194; - 0.066% U(3)O(8) over 1.1 metres, and 0.055% U(3)O(8) over 1.0 metres in hole SP-196; - 0.105% U(3)O(8) over 1.1 metres, and 0.074% U(3)O(8) over 2.8 metres in hole SP-201; - 1.527% U(3)O(8) over 1.5 metres in hole SP-203; - 0.076% U(3)O(8) over 1.6 metres in hole SP-207; - 0.062% U(3)O(8) over 1.0 metres in hole SP-209; - 0.120% U(3)O(8) over 0.7 metres in hole SP-210; - 0.370% U(3)O(8) over 6.5 metres, including 1.131% U(3)O(8) over 2.0 metres, in hole SP-211; - 0.360% U(3)O(8) over 1.0 metres in hole SP-212; and - 0.140% U(3)O(8) over 0.4 metres, and 0.125% U(3)O(8) over 2.7 metres in hole SP-213.
True thickness of mineralization has not yet been determined. Intercepts in drill holes SP-201, 203, 210, 211 and 212 are unconformity-hosted mineralization, while all other intercepts are basement-hosted.
The Telephone drilling has highlighted three anomalously mineralized areas that contain a combination of unconformity-hosted and basement-hosted mineralization. Additional mineralized drilling intercepts are also present periodically along the four-kilometre length of the Telephone Lake trend and extend southward into the Shamus Lake area.
As mineralization is open in many areas, UEX will focus its 2010 winter exploration program to follow up on these results. It is anticipated that this drilling program will commence in mid-January 2010.
Vixen Lake South
In the Vixen Lake South area, which lies 1.5 kilometres northwest of the Raven Deposit, drilling tested the core of a well-defined, east-northeast trending gravity-resistivity low where historical drilling in shallow holes had identified broad areas of clay alteration. Alteration style, geophysical signature and the east-northeast trend of the alteration zones are similar to the signature of alteration associated with the Horseshoe and Raven Deposits. Four drill holes (VU-001 to VU-004, 1,697 metres total) were drilled; no significant mineralization was intersected.
Future Scoping Studies for Horseshoe and Raven
With a high proportion of the Horseshoe and Raven resource base in the Indicated category, UEX will be initiating a scoping level evaluation of the potential economic viability of mining the deposits, which could then be advanced to feasibility level if results are encouraging. These studies will examine the most efficient methods and procedures for extracting the defined uranium resource, including the most appropriate road access and support infrastructure, mining methods, operating plans, cash flow analyses and projections in order to determine net present values and internal rates of return for the deposits at various uranium price levels. In support of such work, environmental baseline studies have been underway since 2006, previously reported metallurgical studies have been completed and initial geotechnical studies have been performed. UEX intends to identify a lead contractor for the scoping and potential feasibility level work in the near future.
2010 Winter Program at Hidden Bay
A budget of
- Telephone Lake - a 20-hole, 6,000-metre diamond drilling program to test potential down dip continuation of known mineralization, to test along strike for extensions of unconformity mineralization, and to test gaps where widely spaced sections have favourable geology for basement-hosted mineralization; and - Shamus grid - a 120 line-kilometre geophysical survey consisting of D.C. resistivity and gravity. This geophysical survey will extend from the southwestern parts of the Telephone Lake area southwesterly to the Hidden Bay property boundary and will test for areas of alteration potentially associated with uranium mineralization. Areas of anomalous alteration and low-grade mineralization have previously been intersected in several drill holes on the Shamus grid and mineralization occurs to the southwest on adjacent properties along the same trend.
In addition to these activities, property-wide compilation and evaluation will continue utilizing previous exploration data.
Maps and other information regarding UEX's exploration projects are available for viewing on UEX's website at www.uex-corporation.com under "Projects".
Sample Handling and Quality Assurance
Geochemical samples are selected with the aid of a hand-held scintillometer to identify areas of above-background radioactivity. Samples are split, with half remaining in the core box, and the remainder shipped to Saskatchewan Research Council Geoanalytical Laboratories ("SRC") where they are crushed and ground to minus 106 microns. The pulp is digested in aqua regia leach and analyzed by ICP for uranium and other elements. In addition to the geochemical analyses, down-hole probe radiometric results obtained for all drill holes on completion of drilling provide an independent check of the geochemical data. UEX systematically inserts sample blanks and standards of several grades into the sample stream. In addition, repeat analyses are routinely analyzed, laboratory standards are inserted by SRC, and selected sample pulps have been submitted to other independent laboratories for check analyses to assess sample repeatability and accuracy of the SRC results.
Technical information in this news release has been reviewed and approved by R. Sierd Eriks, P.Geo., UEX's Vice President of Exploration, and David Rhys, P.Geo., a consultant to UEX, who are Qualified Persons as defined by National Instrument 43-101.
About UEX
UEX is a Canadian uranium exploration and development company actively involved in 19 uranium projects, including seven that are 100% owned and operated by UEX, one joint venture with AREVA that is operated by UEX, ten joint-ventured with AREVA and one under option from JCU (
ON BEHALF OF THE BOARD OF DIRECTORS OF UEX CORPORATION Graham C. Thody President and CEO
Forward-Looking Statements
This news release contains "forward-looking statements" that are based on UEX's current expectations, estimates, forecasts and projections. These forward-looking statements include statements regarding UEX's outlook for our future operations, plans and timing for the commencement or advancement of exploration activities on our properties, and other expectations, intention and plans that are not historical fact. The words "estimates", "projects", "expects", "intends", "believes", "plans", or their negatives or other comparable words and phrases are intended to identify forward-looking statements. Such forward-looking statements are based on certain factors and assumptions and are subject to risks, uncertainties and other factors that could cause actual results to differ materially from future results expressed or implied by such forward-looking statements. Important factors that could cause actual results to differ materially from UEX's expectations include uncertainties relating to interpretation of drill results and geology, continuity and grade of deposits, fluctuations in uranium prices and currency exchange rates, and other risks and uncertainties disclosed in UEX's Annual Information Form and other filings with the securities commission on SEDAR. Many of these factors are beyond the control of UEX. Consequently, all forward-looking statements made in this news release are qualified by this cautionary statement and there can be no assurance that actual results or developments anticipated by UEX will be realized. For the reasons set forth above, investors should not place undue reliance on such forward-looking statements. Except as required by applicable law, UEX disclaims any intention or obligation to update or revise forward-looking information, whether as a result of new information, future events or otherwise.
Table 1 Summer 2009 Hidden Bay Drilling Program Intersections from Drill Holes HU-359 to HU-367, RU-217 to RU-226, SP-191 to SP-216 and VU-001 to VU-004. Only intervals with composite grades greater than 0.02% U(3)O(8) and a grade-thickness product greater than 0.02 are listed below. All analyses were performed by Saskatchewan Research Council by ICP. ------------------------------------------------------------------------- Depth Hole Location of Hole From To Length Avg. Grade (metres) (metres) (metres) (metres) (% U(3)O(8)) ------------------------------------------------------------------------- HU-359 Horseshoe 300.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- HU-360 Horseshoe 300.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- HU-361 Horseshoe 270.0 71.0 72.0 1.0 0.032 120.0 124.0 4.0 0.076 133.0 136.0 3.0 0.107 including 133.4 135.5 2.1 0.140 220.5 223.0 2.5 0.034 ------------------------------------------------------------------------- HU-362 Horseshoe 291.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- HU-363 Horseshoe 639.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- HU-364 Horseshoe 534.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- HU-365 Horseshoe 399.0 271.0 272.0 1.0 0.023 ------------------------------------------------------------------------- HU-366 Horseshoe 324.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- HU-367 Horseshoe 489.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- RU-217 Raven 81.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- RU-218 Raven 72.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- RU-219 Raven 81.0 45.0 48.0 3.0 0.035 including 46.0 47.0 1.0 0.087 ------------------------------------------------------------------------- RU-220 Raven 72.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- RU-221 Raven 81.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- RU-222 Raven 72.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- RU-223 Raven 411.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- RU-224 Raven 549.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- RU-225 Raven 222.0 179.5 180.5 1.0 0.061 183.4 192.6 9.2 0.062 including 187.2 191.6 4.4 0.107 ------------------------------------------------------------------------- RU-226 Raven 219.0 112.0 113.0 1.0 0.040 138.4 143.0 4.6 0.120 ------------------------------------------------------------------------- SP-191 Telephone 349.0 230.0 230.8 0.8 0.030 295.0 297.0 2.0 0.042 including 295.5 296.0 0.5 0.110 325.0 328.0 3.0 0.035 ------------------------------------------------------------------------- SP-192 Telephone 411.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- SP-193 Telephone 369.0 226.0 229.0 3.0 0.020 236.0 238.0 2.0 0.100 252.0 253.9 1.9 0.401 ------------------------------------------------------------------------- SP-194 Telephone 359.0 223.7 224.5 0.8 0.128 including 223.7 224.0 0.3 0.277 270.0 272.5 2.5 0.023 ------------------------------------------------------------------------- SP-195 Telephone 321.0 101.3 102.0 0.7 0.025 291.0 292.0 1.0 0.035 ------------------------------------------------------------------------- SP-196 Telephone 345.0 258.0 259.0 1.0 0.021 314.3 315.4 1.1 0.066 325.0 326.0 1.0 0.055 334.0 336.0 2.0 0.024 ------------------------------------------------------------------------- SP-197 Telephone 398.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- SP-198 Telephone 352.0 310.0 314.0 4.0 0.020 324.0 325.0 1.0 0.022 ------------------------------------------------------------------------- SP-199 Telephone 386.0 298.0 298.5 0.5 0.054 361.0 362.0 1.0 0.027 363.0 364.0 1.0 0.021 376.0 378.0 2.0 0.026 ------------------------------------------------------------------------- SP-200 Telephone 300.0 272.0 273.0 1.0 0.020 ------------------------------------------------------------------------- SP-201 Telephone 300.0 165.0 166.1 1.1 0.105 230.5 234.0 3.5 0.026 239.5 242.3 2.8 0.074 266.0 267.0 1.0 0.031 ------------------------------------------------------------------------- SP-202 Telephone 372.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- SP-203 Telephone 270.0 122.0 123.5 1.5 1.527 252.5 253.0 0.5 0.045 ------------------------------------------------------------------------- SP-204 Telephone 351.0 266.5 267.5 1.0 0.044 ------------------------------------------------------------------------- SP-205 Telephone 343.0 237.0 239.5 2.5 0.030 248.0 250.0 2.0 0.035 ------------------------------------------------------------------------- SP-206 Telephone 351.0 178.0 178.5 0.5 0.045 ------------------------------------------------------------------------- SP-207 Telephone 351.0 279.4 281.0 1.6 0.076 ------------------------------------------------------------------------- SP-208 Telephone 300.0 121.0 122.6 1.6 0.039 137.5 138.0 0.5 0.077 142.5 143.5 1.0 0.021 180.5 181.5 1.0 0.035 ------------------------------------------------------------------------- SP-209 Telephone 348.0 139.0 140.0 1.0 0.020 188.6 189.6 1.0 0.062 200.6 202.6 2.0 0.021 ------------------------------------------------------------------------- SP-210 Telephone 171.0 99.0 103.0 4.0 0.035 including 101.3 102.0 0.7 0.120 ------------------------------------------------------------------------- SP-211 Telephone 180.0 135.0 145.0 10.0 0.245 including 137.5 144.0 6.5 0.370 including 137.5 139.5 2.0 1.131 ------------------------------------------------------------------------- SP-212 Telephone 180.0 140.0 141.0 1.0 0.360 ------------------------------------------------------------------------- SP-213 Telephone 330.0 250.95 252.0 1.05 0.064 including 250.95 251.35 0.4 0.140 259.3 265.0 5.7 0.068 including 259.3 262.0 2.7 0.125 295.0 296.0 1.0 0.027 ------------------------------------------------------------------------- SP-214 Telephone 180.0 136.0 137.0 1.0 0.024 ------------------------------------------------------------------------- SP-215 Telephone 171.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- SP-216 Telephone 180.0 142.0 145.0 3.0 0.028 including 144.0 144.5 0.5 0.090 155.6 156.6 1.0 0.022 ------------------------------------------------------------------------- VU-001 Vixen 391.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- VU-002 Vixen 366.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 ------------------------------------------------------------------------- VU-003 Vixen 549.0 405.0 405.5 0.5 0.043 VU-004 Vixen 391.0 No intervals (greater than) 0.02% U(3)O(8) with grade-thickness (greater than) 0.02 -------------------------------------------------------------------------
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