| | Published : July 21st, 2011 | Extends Areas of Uranium Mineralization at Way Lake |
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News Release - Thursday, July 21, 2011 JNR Extends Areas of Uranium Mineralization at Way Lake
Saskatoon, SK, July 21, 2011 - JNR Resources Inc. (TSXV:JNN) ('JNR' or the 'Company') is pleased to report geoanalytical results from the 2011 winter Diamond drilling program on the Company's 100% owned Way Lake uranium project, located 55 kilometres east of the Key Lake uranium mine in the Athabasca Basin of northern Saskatchewan. Drilling has extended the Fraser Lakes Zone B to the east-northeast, and anomalous U-Th mineralization has been intersected in a new area, Fraser Lakes North.
The 2011 drilling program comprised 2,590 metres in 10 holes. Four holes tested the east-northeast extension of the Fraser Lakes Zone B. Six holes tested ancillary structural/mineralized targets related to the Fraser Lakes Zone B; located within previously untested portions of a folded, 65-km long electromagnetic (EM) graphite-sulfide-rich conductor system. Six of the 10 drill holes intersected anomalous radioactivity accompanied by significantly disrupted and locally clay-altered Wollaston Group graphitic pelitic gneisses and uraniferous granitic pegmatites.
Multiple intervals of uranium and/or thorium (U-Th) mineralization were intersected in four new holes (WYL-11-68, -69, -70, and -71; Table 1) that tested Fraser Lakes Zone B on its east-northeast end. The better U-Th intersections occur in drill holes WYL-11-68, -70 and -71, and are accompanied by highly anomalous concentrations of base metals and rare earth element (REE) enrichment. At a cut-off grade of 0.025% U3O8, the results from WYL-11-68 and -70 are impressive. To date, drilling of this zone has identified an extensive area approximately 1,250 metres long by 650 metres wide of moderately dipping, multiple stacked uranium and thorium mineralized horizons, which are open to the southwest and east-northeast to a depth of at least 175 metres.
Anomalous radioactivity was intersected within a new area, Fraser Lakes North, located 5 kilometres northeast of Fraser Lakes Zone B. Drill holes WYL-11-73 and -74 (Table 1) report low-grade, basement-hosted U-Th mineralization in graphitic pelitic gneisses and granitic pegmatites. These holes also exhibit evidence for major structural reactivation, significant clay alteration, uranium remobilization, and basinal brine fluid circulation.
The exceptional exploration potential of the Fraser Lakes area is further supported by geoanalytical results from PIMA infrared spectroscopy of four holes drilled in the T-Bone Lake area (News Release: June 17, 2010), located 4 kilometres west-southwest of Fraser Lakes North and due north of Fraser Lakes Zone B. These results indicate a preponderance of the important pathfinder mineral, illite, within a major clay-filled fault system that was intersected in 2010.
Dave Billard, Vice-President Exploration and COO for JNR, comments: "These results confirm that the Fraser Lakes district has significant exploration upside, with many targets having the potential to host high-grade uranium mineralization. Geological and geochemical features identified in the Fraser Lakes district show distinct similarities to high-grade, basement-hosted discoveries in the Athabasca basin, such as Cameco's Millennium and Hathor's Roughrider deposits".
Results from the 2011 drilling program continue to demonstrate the significant uranium and metal endowment within the Fraser Lakes district, and will be integrated within on-going exploration models to plan and facilitate JNR's next phase of drilling new targets.
Table 1. Fraser Lakes Area - Significant Drill Results
DDH# |
From (m) |
To (m) |
Width (m) |
U3O8 % |
ThO2 % |
Other Metals (%) |
WYL-11-68 |
164.00 |
166.00 |
2.00 |
0.029 |
0.031 |
Cu-0.015, V-0.012, Zn-0.013 |
|
172.00 |
173.00 |
1.00 |
0.074 |
0.088 |
Cu-0.017, Pb-0.025 |
|
173.50 |
174.50 |
1.00 |
0.035 |
0.039 |
Cu-0.074, Pb-0.011 |
|
209.50 |
211.00 |
1.50 |
0.028 |
|
Anomalous Th, Pb |
|
212.00 |
213.50 |
1.50 |
0.05 |
0.031 |
Pb-0.015 |
|
232.80 |
233.50 |
0.70 |
|
0.034 |
Anomalous U, Cu, Pb, and Zn |
|
281.60 |
282.10 |
0.50 |
0.076 |
0.181 |
Pb-0.02, Zn-0.019 |
|
|
|
|
|
|
|
WYL-11-69 |
135.50 |
136.50 |
1.00 |
0.033 |
0.039 |
Cu-0.012 |
|
137.50 |
138.00 |
0.50 |
|
|
Cu-0.044, V-0.009, Zn-0.008 |
|
|
|
|
|
|
|
WYL-11-70 |
99.50 |
100.00 |
0.50 |
|
0.051 |
Anomalous U |
|
190.50 |
192.50 |
1.50 |
|
|
Cu-0.012, Ni-0.03, V-0.041, Zn-0.065 |
|
198.20 |
199.20 |
1.00 |
0.098 |
0.080 |
Pb-0.024, Zn-0.033 |
|
208.00 |
211.00 |
3.00 |
0.053 |
0.054 |
Mo-0.017, Pb-0.018, V-0.01 |
|
212.80 |
213.80 |
1.00 |
0.038 |
0.029 |
Pb-0.014, Zn-0.012 |
|
214.00 |
214.50 |
0.50 |
0.024 |
|
Anomalous Mo, Th |
|
217.20 |
217.70 |
0.50 |
0.044 |
0.030 |
|
|
218.20 |
218.70 |
0.50 |
0.045 |
0.040 |
Mo-0.019 |
|
220.50 |
221.00 |
0.50 |
0.025 |
0.023 |
|
|
225.40 |
226.40 |
1.00 |
0.036 |
0.049 |
Cu-0.022, Mo-0.013, Zn-0.012 |
|
234.50 |
236.00 |
1.50 |
0.025 |
0.021 |
|
|
260.00 |
262.00 |
2.00 |
0.043 |
0.027 |
Anomalous Pb |
|
|
|
|
|
|
|
WYL-11-71 |
144.50 |
145.50 |
1.00 |
|
0.046 |
|
|
148.00 |
149.50 |
1.50 |
|
|
Anomalous Th, V, Zn |
|
150.50 |
151.00 |
0.50 |
|
0.047 |
Anomalous Mo, U |
|
153.50 |
154.50 |
1.00 |
|
0.028 |
|
|
212.00 |
214.00 |
2.00 |
|
|
Cu-0.031, Ni-0.041, V-0.039, Zn-0.02 |
|
216.50 |
217.50 |
1.00 |
|
|
Cu-0.012, Ni-0.03, V-0.027 |
|
247.00 |
252.50 |
5.50 |
|
|
Cu-0.023, V-0.017, Zn-.014 |
|
287.75 |
288.00 |
0.25 |
|
|
Cu-0.51, V-0.015, Zn-.009 |
|
|
|
|
|
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|
WYL-11-72 |
142.50 |
143.50 |
1.00 |
|
|
Ni-0.023, V-0.024, Zn-0.027 |
|
|
|
|
|
|
|
WYL-11-73 |
135.00 |
135.50 |
0.50 |
|
0.022 |
Anomalous U |
|
197.50 |
203.00 |
5.50 |
|
|
Cu-0.023, Ni-0.039, V-0.041, Zn-0.061 |
including |
197.50 |
199.00 |
1.50 |
0.002 |
0.002 |
Mo-0.01, Ni-0.049, V-0.056, Zn-0.176 |
|
|
|
|
|
|
|
WYL-11-74 |
41.00 |
43.50 |
2.50 |
|
|
Anomalous U, Th |
|
123.00 |
125.50 |
2.50 |
|
|
Cu-0.011, V-0.016, Zn-.015 | Note: All holes were drilled at a 45 to 50 degree angle across the lithostratigraphic/radioactive horizons on sections consisting of at least two drill holes. Widths represent downhole core lengths; true widths cannot be reliably estimated at this time. 0.025% U3O8 and 0.030% ThO2 cut-offs were applied.
JNR's Director of Exploration, Dr. Irvine R. Annesley, PGeo, is the qualified person responsible for the technical data presented in this release. Samples were analyzed at the Saskatchewan Research Council Geoanalytical Laboratories in Saskatoon, SK, a Standards Council of Canada (CCRMP) certified analytical laboratory. All technical information for the Company's exploration projects is obtained and reported under a formal quality assurance and quality control program, details of which are presented on the Company's website at: www.jnrresources.com/s/Glossary.asp.
ON BEHALF OF THE BOARD
Rick Kusmirski President & CEO
For further information contact JNR Resources at 306.382.2211 or 877.567.6463
Neither the 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 news release. Statements contained in this news release that are forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements of the Company to be materially different from any future results, performance or achievements expressed or implied by the forward-looking statements. Such risks and other factors include, among others, risks related to the accessibility to the property; operational risks; weather; availability of equipment and personnel; changes in project parameters as plans continue to be refined; delays in obtaining governmental approvals; delays or failure in obtaining financing on acceptable terms. Although the Company has attempted to identify important factors that could cause actual actions, events or results to differ materially from those described in forward-looking statements, there may be other factors that cause actions, events or results not to be as anticipated, estimated or intended. There can be no assurance that forward-looking statements will prove to be accurate, as actual results and future events could differ materially from those anticipated in such statements. Accordingly, readers should not place undue reliance on forward-looking statements.
You can also view this News Release on our website at: http://www.jnrresources.com/s/NewsReleases.asp?ReportID=468057
Copyright � 2010 JNR Resources Inc. (JNN-TSXV) All rights reserved. For more information visit our website at http://www.jnrresources.com/ or send email to info@jnrresources.com. If you wish to be removed from our email list, .
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ProfileMarket IndicatorsVALUE : Projects & res.Press releasesAnnual reportRISK : Asset profileContact Cpy |
JNR is a silver and gold exploration company based in Canada. JNR holds various exploration projects in Canada. Its main exploration properties are BELL LAKE, PENDLETON LAKE, KELIC LAKE, NORTH WEDGE, SOUTH DUFFERIN, SNOWBIRD PROPERTY, YURCHISON LAKE, TOPSAILS, SOUTH FORK, CRACKINGSTONE, MOORE LAKE, ROCKY BROOK, SOUTH CIGAR, LAZY EDWARD BAY, WAY LAKE, BLACK LAKE PROPERTY and NEWNHAM in Canada. JNR is listed in Canada, in Germany and in United States of America. Its market capitalisation is CA$ 11.5 millions as of today (US$ 11.4 millions, € 8.4 millions). Its stock quote reached its lowest recent point on December 31, 2003 at CA$ 0.03, and its highest recent level on December 31, 2007 at CA$ 4.50. JNR has 114 620 000 shares outstanding. |
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