Rare Element Resources Ltd. Reports Additional 2011 Rare Earth Element and Gold Drilling Results
26.03.2012 | Marketwired
- Confirms Previously Reported HREE-Enrichment TargetsLAKEWOOD, COLORADO -- (Marketwire) -- 03/26/12 -- Rare Element Resources Ltd. (TSX: RES)(NYSE Amex: REE) is pleased to announce rare earth element (REE) and gold assay results from 29 additional drill holes that were completed during the 2011 core drilling program at the Company's 100% owned Bear Lodge property, located in northeastern Wyoming, USA. These results include 15 drill holes from the Bull Hill resource area, six drill holes from the Whitetail Ridge area, four drill holes from the East Taylor target area, and four drill holes from the Carbon target area. Three drill holes from the 2011 program remain to be assayed.
Dr. Jim Clark, Vice President of Exploration for the Company stated, "Our 2011 drilling results confirm the continuity of the mineralized bodies, and we have continued to significantly expand the resource. We are excited about the prospect of delineating another resource that exhibits the potential for higher grades of HREE at Whitetail Ridge, East Taylor and Carbon. We feel that the district has tremendous upside potential."
Bull Hill Resource Area
------------------------------------------
Interval Grade
-------------------- ----------
Drill Hole Feet Meters TREO (%)
RES11-23 51 16 4.35%
RES11-40 20 6 7.13%
RES11-43 133 41 3.44%
RES11-44 98 30 2.25%
RES11-48 97 30 4.58%
55 17 12.35%
27 8 9.44%
RES11-51 108 33 3.32%
RES11-52 59 18 2.64%
RES11-58 384 117 6.45%
78 24 5.14%
RES11-59 43 13 2.40%
57 17 2.24%
Whitetail Ridge Resource Area
----------------------------------------------------
Interval Grade
-------------------- --------------------
Drill Hole Feet Meters TREO (%) Au (g/t)
RES11-15 39 12 2.43%
36 11 3.06%
RES11-29 22 7 2.95%
43 13 2.00%
RES11-34 28 9 3.03%
RES11-47 70 21 0.714
38 12 0.695
RES11-54 163 50 0.750
73 22 1.074
East Taylor Target Area
----------------------------------------------------
Interval Grade
-------------------- --------------------
Drill Hole Feet Meters TREO (%) Au (g/t)
RES11-28 39 12 2.06%
22 7 3.00%
267 81 0.921
RES11-31 36 11 3.86%
186 57 0.810
RES11-32 45 14 2.60%
134 41 0.740
RES11-57 53 16 3.42%
RES11-57A 52 16 3.78%
RES11-60 32 10 3.21%
DRILLING RESULTS
The RE mineralization intersected in the 29 drill holes is contained primarily within the near-surface oxidized (FMR) in fully oxidized but incompletely leached equivalents of carbonatite dikes (oxide carbonate/OxCa). These dikes are widespread in the district and concentrated in dike swarms and stockwork zones on the Bull Hill, Bull Hill West, Whitetail Ridge, East Taylor and Carbon resource and target areas (Figure 1). Overlapping gold mineralization in the Whitetail Ridge, East Taylor and Carbon areas is contained in the FMR and OxCa dikes and stockwork, and in the alkali silicate host rocks. FMR refers to the major constituents of the highly oxidized, former carbonatite dikes that occur in a depth range from surface to 300-500ft/91-152m beneath the surface-F(FeOx)-M(MnOx)-R(REE minerals) (FMR).
Bull Hill Resource Area (now includes Bull Hill West)
Highlights from the Bull Hill area drill holes are summarized below.
Bull Hill Resource Area
Interval Est True Mineralized
From To Intercept Thickness Lithology Grade
--------- -------- --------- ---------- ---------------- --------
Drill Hole Ft M Ft M Ft M Ft M TREO (%)
---------- --- ---- ---- --- ---- ---- ----- ----
Oxide FMR dikes;
FMR, clay veins
RES11-23 124 38 175 53 51 16 17.5 5.3 and stockwork 4.35%
644 196 648 198 4 1 3.5 1.1 Oxide dike 4.35%
845 258 851 259 4 1 2.8 0.9 Oxide dike 4.35%
Oxide dike and
RES11-36 289 88 297 91 8 2 6.2 1.9 stockwork 2.36%
461 141 465 142 4 1 3.1 0.9 Oxide dike 13.89%
506 154 511 156 5 2 3.9 1.2 Oxide dike 2.04%
539 164 550 168 11 3 8.5 2.6 Oxide dike 2.00%
772 235 779 237 7 2 5.4 1.6 Oxide dike 8.62%
FMR dike and
RES11-37 40 12 60 18 20 6 14.0 4.3 stockwork 2.33%
FMR dike and
110 34 134 41 24 7 16.6 5.1 stockwork 2.79%
Oxide dike, FMR
RES11-38 34 10 87 27 54 16 46.5 14.2 and clay veins 2.19%
Oxide FMR dike,
FMR and clay
stockwork and
205 62 274 84 69 21 48.8 14.9 veins 5.40%
Oxide FMR and
clay stockwork
284 87 341 104 57 17 40.3 12.3 and veins 4.88%
Oxide FMR and
clay stockwork
404 123 423 129 19 6 14.6 4.5 and veins 2.44%
521 159 528 161 7 2 5.4 1.6 Oxide FMR dike 12.96%
Oxide FMR dikes
RES11-40 41 12 70 21 30 9 22.7 6.9 and stockwork 2.51%
117 36 137 42 20 6 14.1 4.3 Oxide FMR dike 7.13%
Oxide FMR
stockwork; clay
320 98 324 99 5 2 3.2 1.0 veins 2.69%
Oxide FMR dike
RES11-41 581 177 588 179 7 2 6.1 1.9 and veins 2.83%
Oxide FMR dikes
607 185 624 190 17 5 16 4.9 and stockwork 2.41%
667 203 671 205 4 1 3.8 1.2 Oxide FMR dike 8.80%
Oxide FMR
RES11-43 224 68 238 73 14 4 9.9 3.0 stockwork 2.31%
Oxide FMR dike
288 88 309 94 21 6 14.8 4.5 and stockwork 3.38%
Oxide FMR veins
452 138 458 140 6 2 5.22 1.6 and stockwork 3.07%
Oxide FMR dikes,
476 145 609 186 133 41 94 28.7 veins, stockwork 3.44%
Oxide FMR
672 205 698 213 26 8 18.4 5.6 stockwork 2.17%
722 220 828 252 106 32 92.2 28.1 Ox-Ca dikes 2.48%
Ox-Ca dikes,
960 293 1033 315 73 22 56.2 17.1 veins, stockwork 2.04%
Oxide FMR
RES11-44 20 6 118 36 98 30 69.3 21.1 stockwork 2.25%
213 65 223 68 10 3 6.7 2.0 Ox-Ca stockwork 2.59%
Eight of the 15 holes in the Bull Hill Resource Area were drilled along a prescribed NE-SW grid at azimuths of 045 degrees and 225 degrees. Holes were also drilled along azimuths of 090 degrees (one hole), 270 degrees (two holes), and 270 degrees (four holes) in order to test for mineralized bodies directed along structures divergent from the main trend of mineralization (Figure 1).
Whitetail Ridge Resource Area
RE mineralization in and adjacent to the Whitetail Ridge Resource Area occurs dominantly NW-trending dikes, veins and stockwork zones. The six holes were drilled along a prescribed NE-SW grid at azimuths of 045 degrees or 225 degrees. The highlights from the Whitetail Ridge area drill holes are summarized in the following table. Two of the drill holes contain significant intercepts of gold mineralization hosted in FMR stockwork and diatreme breccia.
Whitetail Ridge Resource Area
Interval Est True Mineralized
From To Intercept Thickness Lithology Grade
--------- -------- --------- ---------- ------------ -----
TREO
Drill Hole ft m ft m ft m ft m (%)
---------- ---- --- ---- --- ---- ---- ----- ----
Ox-Ca
RES11-15 290 88 328 100 39 12 38.5 11.7 stockwork 2.43%
Ox-Ca
393 120 402 123 9 3 9 2.7 stockwork 2.28%
Ox-Ca dikes
and
459 140 495 151 36 11 36 11.0 stockwork 3.06%
565 172 590 180 25 8 25 7.6 Ox-Ca dike 3.55%
813 248 819 250 6 2 6 1.8 Ox-Ca dike 2.37%
Oxide dike
RES11-29 35 11 57 17 22 7 20 6.1 and veins 2.95%
97 30 107 33 10 3 9 2.7 Oxide veins 4.46%
Oxide
stockwork
147 45 190 58 43 13 33 10.1 and veins 2.00%
Ox-Ca dike
594 181 609 186 11 3 7.8 2.4 and veins 2.33%
661 201 666 203 5 2 2.9 0.9 Ox-Ca dike 2.79%
Oxide
RES11-34 226 69 276 84 10 3 10 3.0 stockwork 2.65%
Oxide dikes
and
806 246 834 254 28 9 19.8 6.0 stockwork 3.03%
Ox-Ca veins
and
RES11-47 638 194 645 197 7 2 4.6 1.4 stockwork 2.49%
Oxide dike
and
955 291 966 294 11 3 7.8 2.4 stockwork 2.10%
Grade Au
(g/t)
--------
Diatreme
breccia with
450 137 520 158 70 21 49.5 15.1 Ox-Ca veins 0.071
Diatreme
breccia with
770 235 808 246 38 12 26.9 8.2 Ox-Ca veins 0.695
RES11-53 406 124 411 125 6 2 3.9 1.2 Ox-Ca dike 2.33%
Diatreme
Breccia with
RES11-54 322 98 335 102 13 4 9.0 2.7 FMR veins 2.69%
720 219 724 221 4 1 2.8 0.9 Ox-Ca vein 4.46%
Diatreme
Breccia with
180 55 190 58 10 3 7.0 2.1 FMR veins 2.010
Diatreme
Breccia with
241 73 404 123 163 50 115.0 35.1 FMR veins 0.750
Diatreme
Breccia with
1090 332 1162 354 73 22 51.0 15.5 Ox-Ca veins 1.074
East Taylor Target Area
The East Taylor target is located approximately 2,500ft/760m west of the main Bull Hill RE deposit and 2,500ft/760m southwest of the Whitetail Ridge deposit (Figure 1). The zone appears to have an easterly strike, as opposed to the dominant northwesterly and northerly mineralized structures in the Bull Hill-Whitetail Ridge deposits. Preliminary geological mapping and projection of FMR intercepts in drill holes suggest that the REE mineralization consists of dikes and adjacent stockwork with dimensions of more than 700ft/210m east-west by 250ft/75m north-south, and the mineralization is open to the east. Results from six core drill holes drilled at the East Taylor target area are reported here and augment the results from the three core holes reported in a 4 August 2011 press release. The core holes were drilled to follow up results from reverse circulation drill hole SUN-090. This hole was collared east of Taylor Ridge during the 2010 gold drilling program and intersected significant FMR-style mineralization strongly enriched in both light and heavy REE (see press release dated 27 October 2011. The REE mineralization is associated with coincident and peripheral zones of gold mineralization, and the gold assay results are also reported here.
East Taylor Target Area
Interval Est True Mineralized
From To Intercept Thickness Lithology Grade
-------- ------- --------- --------- -------------- ------
TREO
Drill Hole ft m ft m ft m ft m (%)
---------- --- --- --- --- ---- ---- ---- ----
Oxide FMR
dike, veins
RES11-28 106 32 144 44 39 12 33.5 10.2 and stockwork 2.06%
Oxide FMR
dike, veins
201 61 214 65 13 4 10.9 3.3 and stockwork 2.96%
Oxide FMR
dike, veins
255 78 277 84 22 7 19.1 5.8 and stockwork 3.00%
Oxide FMR
dike, veins
RES11-31 8 2 44 13 36 11 25.5 7.8 and stockwork 3.86%
FMR dikes and
RES11-32 19 6 64 20 45 14 42 12.8 stockwork 2.60%
86 26 107 33 21 6 19.7 6.0 Stockwork 2.76%
274 84 279 85 6 2 5 1.5 FMR dike 2.41%
Grade Au
(g/t)
--------
FMR dikes and
6 2 140 43 134 41 126 38.4 stockwork in Trachyte 0.740
FMR dikes and
RES11-33 0 0 143 44 143 44 101 30.8 stockwork in Trachyte 0.500
Carbon Target Area
The Carbon REE target is located approximately 1,200 ft/370m northwest of the Whitetail Ridge deposit along an apparent northwest-trending zone of mineralization (Figure 1). Two reverse-circulation drill holes (SUN-076 and SUN-079) were completed during the 2010 Sundance gold exploration program and cut significant REE mineralization in FMR and unoxidized carbonatite vein material (see news release dated 4 August 2011). The REE mineralization may portend the northwestern extension of the Whitetail Ridge system or, alternatively, a distinct FMR/carbonatite mineralized system. Significant REE-bearing intercepts from the Carbon target area are summarized below. If this mineralization is a continuation of the Whitetail Ridge dike system and the Bull Hill SW system, it may strike up to 5,000ft/1,500m in length. The Carbon target exhibits enrichment in both light and heavy REEs.
Carbon REE Target Area
Interval Est True Mineralized
From To Intercept Thickness Lithology Grade
--------- --------- --------- ---------- -------------- --------
Drill Hole ft m ft m ft m ft m TREO (%)
---------- ---- ---- ---- ---- ---- ---- ----- ----
RES11-56 16 5 26 8 10 3 7.1 2.2 Ox-Ca dike 4.74%
330 101 334 102 4 1 2.8 0.9 Ox-Ca dike 3.88%
Ox-Ca dike and
RES11-57 19 6 72 22 53 16 46 14.0 stockwork 3.42%
RES11-58A 19 6 71 22 52 16 25.8 7.9 Ox-Ca dike 3.78%
531 162 541 165 10 3 7.1 2.2 Oxide FMR dike 3.56%
Oxide and Ox-
RES11-60 76 23 108 33 32 10 22.6 6.9 Ca dike 3.21%
Heavy Rare Earth Enrichment
In 2011, the Company identified significant HREE enrichment in FMR and oxide-carbonate carbonatite dikes at the Whitetail Ridge resource area and the East Taylor and Carbon target areas (see news releases dated 4 August and 27 October 2011). The assay results reported here confirm those observations. Preliminary mineralogical studies indicate that the Y-HREE (yttrium-heavy rare earth element) mineralization is found primarily in the RE fluocarbonates, synchysite and parasite, at Whitetail Ridge and Carbon, and in xenotime, and yttrium-vanadiam phosphate, and RE fluocarbonates at East Taylor. Individual RE assays for Eu, Tb, Dy and Y in intercepts greater than 20ft/6.1m from drill holes reported here are summarized below. Values from the Bull Hill Measured and Indicated resource is included for comparison.
Assay Summary for HREEs in Selected Drill Hole Intercepts
Interval
From To Intercept
-------- ------- ---------
Location
and Drill
Hole ft m ft m ft m % TREO % Eu2O3 % Tb2O3 % Dy2O3 % Y2O3
---- --- --- --- ---- ---- ------- ------- ------- ------- -------
Bull Hill
M&I (For comparison) 3.840% 0.022% 0.004% 0.012% 0.043%
Whitetail Ridge
RES11-15 290 88 328 100 39 12 2.430% 0.020% 0.006% 0.019% 0.048%
459 140 495 151 36 11 3.060% 0.027% 0.008% 0.029% 0.061%
565 172 590 180 25 8 3.550% 0.030% 0.008% 0.031% 0.085%
RES11-29 35 11 57 17 22 7 2.950% 0.024% 0.006% 0.018% 0.036%
147 45 190 58 43 13 2.000% 0.023% 0.006% 0.020% 0.050%
RES11-34 806 246 834 254 28 9 3.030% 0.018% 0.004% 0.012% 0.038%
Carbon
RES11-57 19 6 72 22 53 16 3.420% 0.030% 0.009% 0.037% 0.134%
RES11-57A 19 6 71 22 52 16 3.780% 0.035% 0.010% 0.044% 0.164%
RES11-60 76 23 108 33 32 10 3.210% 0.029% 0.008% 0.034% 0.130%
East Taylor
RES11-28 106 32 144 44 39 12 2.060% 0.022% 0.008% 0.031% 0.100%
255 78 277 84 22 7 3.000% 0.030% 0.013% 0.049% 0.166%
RES11-31 8 2 44 13 36 11 3.860% 0.050% 0.017% 0.064% 0.166%
RES11-32 19 6 64 20 45 14 2.600% 0.028% 0.010% 0.039% 0.108%
86 26 107 33 21 6 2.760% 0.026% 0.013% 0.060% 0.193
The grades for Eu, Tb, Dy and Y are among the highest of any North American REE deposit.
REE assay values are reported by convention as the combined oxide equivalents (REO) of the 15 elements in the lanthanide series plus yttrium. The Bull Hill deposits at the Bear Lodge project contain predominately the light REEs (lanthanum, cerium, praseodymium, neodymium and samarium), with economically important quantities of several of the heavy REEs (europium, dysprosium and terbium). The Whitetail Ridge Resource area and the East Taylor and Carbon target areas have more abundant HREE enrichment, with enhanced abundances of Eu, Dy, Tb and Y (see news release dated 4 August 2011).
For additional information regarding the metallurgy of our deposits, please refer to press releases dated 15 March 2012, 1 March 2012 and 7 September 2011.
To view Figure 1 (Drill hole location map), please visit the following link: http://media3.marketwire.com/docs/RES326F1.pdf
Assays, Quality Control and Standard Certification
ALS Chemex conducted the assaying for the REEs reported here in their Vancouver, BC assay facility. ALS Chemex Vancouver is accredited to ISO 9001 and operates according to ALS Group standards consistent with ISO 17025 methods at other laboratories. The samples were prepared and subjected to lithium metaborate fusion, followed by ICP analysis and a mass spectroscopy finish.
Analytical quality is monitored through the use of randomly inserted quality control samples, including standards, blanks and duplicates, which are blinded to the analytical laboratory. Results from the analyses at ALS Chemex are evaluated continuously by Dr. Jeffrey Jaacks, the Company's QA/QC consultant, who is a Qualified Person according to National Instrument 43-101. The results from the current data set indicate acceptable accuracy and precision. Blank analyses also indicate no issues with carry-over contamination.
Rare Element Resources Ltd. (TSX: RES)(NYSE Amex: REE) is a publicly traded mineral resource company focused on exploration and development of rare-earth elements and gold on the Bear Lodge property.
REEs are key components of the green energy technologies and other high-technology applications. Some of the major applications include hybrid automobiles, plug-in electric automobiles, advanced wind turbines, computer hard drives, compact fluorescent light bulbs, metal alloys, additives in ceramics and glass, petroleum cracking catalysts and a number of critical military applications. China currently produces more than 95% of the 130,000 tonnes of REEs consumed annually worldwide, and China has been reducing its exports of REEs each year. The REE market is growing rapidly, and is projected to accelerate if the green technologies are implemented on a broad scale.
ON BEHALF OF MANAGEMENT
James G. Clark, Ph.D.
Vice President Exploration
For information, refer to the Company's website at www.rareelementresources.com.
Donald E. Ranta, PhD, PGeo, serves the Board of Directors of the Company as an internal, technically Qualified Person. Technical information in this news release has been reviewed by Dr. Ranta and has been prepared in accordance with Canadian regulatory requirements that are set out in National Instrument 43-101. This news release was prepared by Company management, who take full responsibility for content.
Forward-Looking Statements
Except for statements of historical fact, certain information contained herein constitutes forward-looking statements. Forward looking statements are usually identified by our use of certain terminology, including "will", "believes", "may", "expects", "should", "seeks", "anticipates", "has potential to", or "intends" or by discussions of strategy or intentions. Such forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results or achievements to be materially different from any future results or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts, and include but are not limited to, statements regarding our expectations regarding future mineral resource estimates; our plans, objectives and expectations with respect to the Bear Lodge Project; general industry and macroeconomic growth rates and statements regarding future performance.
Forward-looking statements used in this discussion are subject to various risks and uncertainties, most of which are difficult to predict and generally beyond the control of the Company. Forward-looking statements in this document are not a prediction of future events or circumstances, and those future events or circumstances may not occur. If risks or uncertainties materialize, or if underlying assumptions prove incorrect, our actual results may vary materially from those expected, estimated or projected. Important factors than can cause the Company's actual results to differ materially from those anticipated in the forward-looking statements include risks associated with commodity prices, exploration results, governmental and environmental regulations, permitting, licensing and approval processes for our operations and other factors described under the heading "Risk Factors" in our Annual Report on Form 10-K for the year ended June 30, 2011, filed with the U.S. Securities and Exchange Commission ("SEC") as updated by our subsequent filings with the SEC. Given these uncertainties, users of the information included herein, including investors and prospective investors, are cautioned not to place undue reliance on such forward-looking statements. The Company undertakes no obligation to update any forward-looking statements made in this press release to reflect future events or developments, except as required by U.S. and Canadian securities laws.
Mineral Resources are not Reserves
Mineral resources that are not mineral reserves do not have demonstrated economic viability. Mineral resource estimates do not account for minability, selectivity, mining loss, and dilution. These mineral resource estimates are in the measured, indicated, and inferred mineral resource categories. Inferred mineral resources are normally considered too speculative geologically for the application of economic considerations that would enable them to be categorized as mineral reserves. There is also no certainty that these inferred mineral resources will be converted to measured and indicated mineral resource categories through further drilling, or into mineral reserves once economic considerations are applied.
Neither TSX Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Exchange) accepts responsibility for the adequacy or accuracy of this release.
Contacts:
Rare Element Resources Ltd.
Anne Hite
Director of Investor Relations
(720) 278-2466
ahite@rarelementresources.com
www.rareelementresources.com
