VR reports 299 metre intersection of Critical metals and REE’s in the first of five drills holes completed in October at Hecla-Kilmer NR-21-22
VR RESOURCES LTD.
1500 – 409 Granville St.
Vancouver, BC, Canada, V6C 1T2
Tel: 604-262-1104; [email protected]
TSX.V: VRR; www.vrr.ca
VR reports 299 metre intersection of Critical metals and REE’s
in the first of five drills holes completed in October at Hecla-Kilmer
NR-21-22
November 1 7, 2021 , Vancouver, B.C.: VR Resources Ltd. (TSX.V: VRR , FSE: 5VR; OTC QB: VRRCF ), the
"Company", or “VR”, is pleased to provide new data from the first of five holes completed in October at
its Hecla-Kilmer (“H-K”) project in northern Ontario. A 299 m intersection in drill hole HK21-005, starting
near surface, confirms the discovery of a new and large-footprint REE and Critical Metals system at H-K:
Total rare earth oxides (TREO(1)) average 0.47 % TREO over 299.53 metres starting near surface
at 52 metres hole depth, just 8 metres below the base of till, and include:
o TREO up to 1.70 % over 3 m from 156 m, within 28 m of 0.80 % TREO starting at 152 m;
o Middle and Heavy rare earth oxides (MHREO(2)) of up to 0.18% over 3 m at 152 m.
Concentrations of the critical metal niobium of 0.20% Nb2O5 over 237.46 m, including:
o 55 m at 0.23% Nb2O5 and 25.4 ppm Ta2O5 from 183 m;
o 31 m at 0.31% Nb2O5 and 33.4 ppm Ta2O5 from 275 m.
Table 1 below provides a summary of results to-date from the reconnaissance drilling at H-K.
Drill hole
From
(m)
To
(m)
Length
(m)
TREO(1)
(%)
MHREO(2)
(%) MH-T(3) Li2O
(ppm)
Nb2O5
(%)
Ta2O5
(ppm)
ThO2
(ppm)
HK21-005 New 52 351.53 299.53 0.47 0.04 8.6% 94 0.18 23.8 135
including New 80.75 318.21 237.46 0.49 0.04 8.2% 91 0.20 27.3 149
including New 152 180 28 0.80 0.08 9.7% 72 0.17 26.5 252
including New 156 159 3 1.70 0.18 10.3% 52 0.08 16.1 562
including New 183 238 55 0.44 0.03 7.5% 106 0.23 25.4 123
including New 186 190 4 0.61 0.04 6.9% 114 0.42 28.2 159
including New 275 306 31 0.61 0.04 6.0% 102 0.31 33.4 215
including New 299 306 7 0.86 0.06 6.6% 90 0.42 45.5 330
HK20-002 NR-21-17 159.60 183 23.4 0.63 0.06 9.9% 427 0.05 8.3 152
NR-21-17 553 606 53.00 0.51 0.05 9.1% 130 0.12 17.1 390
including NR-21-17 566.65 585 18.35 0.67 0.07 9.4% 114 0.14 18.8 548
HK20-004 NR-21-20 40.30 98.40 58.10 0.38 0.04 11% 107 0.15 25.37 155
including NR-21-20 57 60.21 3.21 1.44 0.15 10% 119 0.17 25.20 438
including NR-21-20 67.23 78 10.77 0.35 0.04 11% 82 0.27 50.12 259
(1) TREO is the summation of Ce2O3 + La2O3 + Pr2O3 + Nd2O3 + Sm2O3 + Eu2O3 + Gd2O3 + Tb2O3 + Dy2O3 + Ho2O3
+ Er2O3 + Tm2O3 + Yb2O3 + Lu2O3 + Y2O3
(2) MHREO is the sum of the middle and heavy rare earth oxides (Sm2O3 + Eu2O3 + Gd2O3 + Tb2O3 + Dy2O3 + Ho2O3
+ Er2O3 + Tm2O3 + Yb2O3 + Lu2O3 + Y2O3)
(3) MH-T is MHREO divided by TREO, expressed as a percent.
Figure 1 shows the key intersections and drill collar locations for the nine drill holes completed to date at
H-K. The four drill holes completed in 2020 targeted the MVI (total magnetic vectorization) anomaly, and
discovered rare earth element (“REE”) and critical metal mineralization over 50 m widths (see data in
VR RESOURCES LTD.
1500 – 409 Granville St.
Vancouver, BC, Canada, V6C 1T2
Tel: 604-262-1104; [email protected]
TSX.V: VRR; www.vrr.ca
Table 1, and drill core photo in Figure 3). T he five follow-up drill holes completed last month, the first of
which is reported on herein, with the remaining holes to be reported on when final geochemical data are
received, focused on the high contrast, 3.5 mGal gravity anomaly that is co-spatial with, but offset from,
the MVI magnetic anomaly targeted in 2020 . The 299 m intersection in Hole 005 is in the east- central
part of the gravity anomaly.
H-K is Confirmed as a new REE and Critical Metal System in Canada
The new data from drill hole HK21-005 confirms the discovery of rare earth elements (“REE”) and critical
metals, for example, niobium and lithium, by the first round of reconnaissance drilling in 2020 (drill hole
HK20-002 reported in July in NR-21-17, and; drill hole HK20-004 reported in October in NR-21-20). Drill
hole HK21-005 confirms a strengthening of the mineral system within the main gravity anomaly.
Scale is important. Figure 1 shows the breadth of mineralization already evident in the early-stage drilling
at H-K. Shown are niobium intersections for drill holes 002, 004 and 005 based on geochemical data in -
hand, and for hole 003 based on XRF data. Also shown are the breadth of intersections of carbonatite
dykes (phoscorite) which are logged in the remaining 2021 drill holes, and which host the REE minerals.
Drill holes 002 and 004 are 200 m etres apart, with mineralization at surface and spanning more
than 500 vertical metres;
Mineralization in Hole 005 spans 299 metres of drill core through the central and eastern part of
the gravity anomaly which itself measures 400 x 800 metres in size;
Mineralization observed in drill core and evident in XRF mineral scans in Holes 008 and 009, for
which geochemical data are not yet in hand, are separated by approximately 1,000 metres along
the long axis of the gravity anomaly.
Figure 2. Graphic log showing new geochemical data for Hole 005, including total rare earth oxide (TREO),
medium to heavy rare earth oxide (MHREO), and the critical metals niobium and tantalum (Nb-Ta).
Figure 3. The key minerals which host the REE’s at H -K include monazite, bastnaesite, fluorapat ite and
apatite, and pyrochlore for niobium. The m ineralization is hosted in sulfide -bearing carbonatite dykes
(phoscorite), fluorite -carbonate vein breccia and hydrothermal breccia. Drill holes 004 and 005 are
overprinted by a high temperature , calc-potassic alteration assemblage which starts at surface and
includes magnetite, biotite and amphibole.
Comment from the CEO
From VR’s CEO Dr. Michael Gunning “These new data confirm and expand upon the potential significance
of the REE and critical metal component of the hydrothermal breccia system at H-K as first discovered in
our reconnaissance drilling last year.
Despite the very early stage of our drilling, four different styles of mineralization are already evident at
H-K: 1. REE + Nb in veined and brecciated carbonatite dykes; 2. lithium mineralization in hydrothermal
breccia; 3. copper sulfide in veinlets with iron and silica, and; 4. elevated secondary gold in porphyry dykes.
Of these, it is already clear that the REE + Nb component of the hydrothermal system at H-K has significant
potential value based on: 1. the vertical and lateral scale represented by t he early intersections ; 2. the
polymetallic signature including niobium, light and heavy rare earth elements, and; 3. TREO concentrations
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over a 299 m intersection are similar to the average grades reported for many REE deposits globally ,
bolstered by a niobium signature achieving 0.2% over a full 237m within that interval.
For those shareholders more accustomed to gold or copper, a value metric for the significance of the
299 m intersection in Hole 5 includes: 0.2% Nb205 = 1.45 g/t gold or 1.9 % copper at equivalent prices of
US$1750/oz gold and US$4.3/kg copper based on current metal values (e.g. Kitco.com, metalary.com).
Mineralogy is also important. Monazite is a key mineral host to the REE’s at H-K. Extraction from monazite
is proven, and facilities are expanding in North America; H-K is aligned with current industry developments,
and with policy statements from governments across North America regarding the desire for domestic
supply of the rare earth elements and critical metals for the transition beyond a fossil fuel- based economy.
Location is just as important, in terms of those REE and critical metal projects and deposits which are
advanced, and those which are not. I want to remind our shareholders to read t he first paragraph of the
“About Hecla-Kilmer” section at the end of this news release in order to appreciate where this project is
located with respect to provincial rail, power and highway infrastructure.
Our drilling to date, and this new geochemical data, are just the starting point for a mineral system and
host multiphase complex of the scale and metal diversity seen at H-K. We will have a more accurate picture
for the potential of all four styles of mineralization at H-K, especially the copper and gold, when: 1. we
have all of the geochemical and mineral data in hand from all nine holes completed to date on the northern
magnetic and gravity anomaly, and; 2. we have completed additional reconnaissance drilling on the larger
magnetic anomaly located 2 – 3 km to the south of the current drilling, on the southern margin of the
complex. To be certain, we have only just begun to delineate mineralization associated with the large
gravity anomaly, and the remainder of this very large complex has yet to be drill-tested, period.
We look forward to providing further updates as we receive additional geochemical data from the
remaining drill holes completed in October , receive proprietary AI analyses of XRF mineral data, and
complete 3-D models integrating new magnetic, density and structural data from drill core.”
Background
Hecla-Kilmer (“H-K”) is a large and multiphase alkaline intrusive complex with carbonatite which is
4 – 6 km in diameter. It is Proterozoic in age, and was emplaced along the western margin of the crustal-
scale Kapuskasing structural zone which bisects the Archean Superior Craton in northern Ontario.
A shallow, six -hole diamond drill program was completed in 1970 as part of a regional base metal
exploration program by Ashland Oil and Elgin Petroleum. One hole was abandoned, and a scant 854 m
were completed in total in the other 5 holes, all on magnetic highs in the outer concentric zones of the
complex. No geochemical sampling or data are reported. Selco Exploration Company completed two drill
holes in 1981 on peripheral magnetic highs as part of a regional diamond exploration program ; they
intersected ultra-basic rocks and breccias peripheral to the outer, concentric zones of the multiphase H-K
complex. A regional airborne magnetic survey covering H -K was completed in 1993 for diamond
exploration, after the early drilling at H -K; it provides high resolution detail of a concentrically zoned
magnetic anomaly at H-K.
The opportunity for VR is to be the first company to apply modern IOCG and carbonatite mineral deposit
models to explore the multiphase H-K complex and hydrothermal breccia system as a whole, and to use
VR RESOURCES LTD.
1500 – 409 Granville St.
Vancouver, BC, Canada, V6C 1T2
Tel: 604-262-1104; [email protected]
TSX.V: VRR; www.vrr.ca
new exploration technologies not previously available when the historic drilling was done. VR completed
the first airborne EM survey over H-K in June, 2020, using the state-of-the-art VTEM+ system of Geotech
Ltd. Flown at 100 m line spacing over a 6 x 7 km survey block for a total of 450 line-km, the data provide
a high resolution of detail. The Company also had an independent, 3 -D inversion of both magnetic and
EM data completed for improved modeling. Finally, a ground -based gravity survey covering an area of
1.5 x 3.5 km was completed in the winter season of 2021, with high-resolution data generated from 597
stations on an equant grid spacing of 100 m . The reader is referred to NR -20-08 dated June 18th, 2020,
for photographs of magnetite-copper-fluorite vein and vein breccia replacement in core from the historic
1970 drill holes located around the periphery of the new gravity anomaly delineated by VR, and gold grains
retrieved from drill core rubble. Current exploration by VR is utilizing this newly acquired geophysical data
to both explore for the source of the copper and gold in the historic core rubble, and to expand upon on
the new discovery of REE and Critical Metals in our first-pass drilling in 2020 and 2021.
Technical Information
Summary technical and geological information for the Company’s various exploration properties is
available at the Company’s website at www.vrr.ca.
VR submit ted all drill core for GeologicAI XRF and SWIR scanning and sawn drill core samples for
geochemical assay to the ALS Global Ltd. (“ ALS”) laboratory facilities in Timmins , Ontario, with final
geochemical analytical work done at the ALS laboratory located in North Vancouver, BC., including lithium
borate fusion, ICP -MS and ICP -AES analyses for base metals, trace elements and full- suite REE analysis,
and gold determination by atomic absorption on fire assay . Analytical results are subject to industry -
standard and NI 43-101 compliant QAQC sample procedures externally by the Company and internally at
the laboratory as described by ALS. Samples from HK20-002 reported on July 22nd, 2021 were sent to SGS
Canada Inc. with a comparable procedure and analysis, as described in previous news releases.
Technical information for this news release has been prepared in accordance with the Canadian regulatory
requirements set out in National Instrument 43-101. Justin Daley, P.Geo., Exploration Manager and Chief
Geologist at VR and a non-independent Qualified Person oversees and/or participates in all aspects of the
Company’s mineral exploration projects, and the content of this news release has been reviewed on
behalf of the Company by the CEO, Dr. Michael Gunning, P.Geo., a non-independent Qualified Person.
About Hecla-Kilmer
The Hecla-Kilmer complex is located 35 k m southwest of the Company’s Ranoke property in northern
Ontario. It is located 23 km northwest of the Ontario hydro-electric facility at Otter Rapids, the Ontario
Northland Railway, and the northern terminus of Highway 634 which links the region to the towns of
Cochrane and Kapuskasing along the northern Trans-Canada Highway located some 100 km to the south.
The H-K property is large. It consists of 224 mineral claims in one contiguous block approximately 6 x 7
km in size and covering 4,617 hectares. The property is owned 100% by VR. There are no underlying
annual lease payments on the property, nor are there any joint venture or back -in interests. There is an
industry-standard royalty attached to the property, including a buy-back provision in favour of VR.
Like the Ranoke property, H-K is located on provincial crown land, with mineral rights administered by the
provincial Ontario Ministry of Northern Development and Mines (MNDM). There are no annual payments,
VR RESOURCES LTD.
1500 – 409 Granville St.
Vancouver, BC, Canada, V6C 1T2
Tel: 604-262-1104; [email protected]
TSX.V: VRR; www.vrr.ca
but the MNDM requires certain annual exploration expenditures and reporting. The property falls within
the traditional territories of the Moose Cree and Taykwa Tagamou First Nations.
About VR Resources
VR is an established junior exploration company focused on greenfields opportunities in copper and gold
(TSX.V: VRR; Frankfurt: 5VR; OTC QB: VRRCF). VR is the continuance of 4 years of active exploration in
Nevada by a Vancouver -based private company. The diverse experience and proven track record of its
Board in early-stage exploration, discovery and M&A is the foundation of VR. The Comp any focuses on
underexplored, large-footprint mineral systems in the western United States and Canada, and is well
financed for its exploration strategies and corporate obligations. VR owns its properties outright, and
evaluates new opportunities on an ongoing basis, whether by staking or acquisition.
The Company continues its normal course of business in 2021 within the framework of modified
exploration programs in response to the COVID -19 pandemic, with the goal of ensuring the health and
safety of staff and project personnel.
ON BEHALF OF THE BOARD OF DIRECTORS:
“Michael H. Gunning”
____________________________
Dr. Michael H. Gunning, PhD, PGeo
President & CEO
For general information please use the following:
Website: www.vrr.ca
Email: [email protected]
Phone: 604-262-1104
Forward Looking Statements
This press release contains forward -looking statements. Forward -looking statements are typically
identified by words such as: believe, expect, anticipate, intend, estimate, postulate and similar
expressions or those which, by their nature, refer to future events. Forward looking statem ents in this
release include “The new data from drill ho le HK21 -005 confirm the discovery of rare earth elements
(“REE”) and critical metals ”, “We look forward to providing further updates as we receive additional
geochemical data from the remaining drill holes completed in October ” and “VR evaluates new
opportunities on an ongoing basis, whether by staking or acquisition.”
This news release contains statements and/or information with respect to mineral properties and/or
deposits which are adjacent to and/or potentially similar to the Company’s mineral properties, but which
the Company has no interest in nor rights to explore. Readers are cautioned that mineral deposits on
similar properties are not necessarily indicative of mineral deposits on the Company’s properties.
VR RESOURCES LTD.
1500 – 409 Granville St.
Vancouver, BC, Canada, V6C 1T2
Tel: 604-262-1104; [email protected]
TSX.V: VRR; www.vrr.ca
Although the Company believes that the use of such statements is reasonable, there can be no assurance
that such statements will prove to be accurate, and actual results and future events could differ materially
from those anticipated in such statements. The Company cautions investors that any forward-looking
statements by the Company are not guarantees of future performance, and that actual results may differ
materially from those in forward-looking statements. Trading in the securities of the Company should be
considered highly speculati ve. All of the Company’s public disclosure filings may be accessed via
www.sedar.com and readers are urged to review these materials.
Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in Policies of the TSX Venture Exchange) accepts
responsibility for the adequacy or accuracy of this release.
VR RESOURCES LTD.
1500 – 409 Granville St.
Vancouver, BC, Canada, V6C 1T2
Tel: 604-262-1104; [email protected]
TSX.V: VRR; www.vrr.ca
Figure 1. Key intersections and drill collar locations for the nine drill holes completed by VR at H-K in 2020 and
2021, plotted on an RTP magnetic base map. Shown in contours are the main magnetic anomalies from the 3D MVI
inversion model of the magnetic data. Shown in shaded outline is the 3.5 mGal residual gravity anomaly derived
from the ground-based gravity survey completed in March, 2020. Drilling in 2021 tested the gravity anomaly, to
augment the drilling in 2020 which targeted the MVI magnetic anomalies.
VR RESOURCES LTD.
1500 – 409 Granville St.
Vancouver, BC, Canada, V6C 1T2
Tel: 604-262-1104; [email protected]
TSX.V: VRR; www.vrr.ca
Figure 2. Downhole graphic log of REE assemblages TREO and MHREO, along with critical metals Nb2O5 and Ta2O5,
in top 400m of drill hole HK21-005 collared within the 3.5 mGal gravity anomaly at H-K. The highest grade REE
mineralization occurs on the outer margins of a core of elevated Nb -Ta mineralization that is centred on a
porphyry syenite dyke emplaced along a major structure evident in magnetic data. The same mineralogical
relationship is shown in drill core in Figure 3 below.