Eloro Resources Ltd. Announces Start of Underground Preparation for Diamond Drilling Program at Iska Iska Silver- Polymetallic Property Area, Potosi Department, Southern Bolivia
NEWS RELEASE | JUNE 25, 2020
Eloro Resources Ltd. Announces Start of Underground
Preparation for Diamond Drilling Program at Iska Iska Silver-
Polymetallic Property Area, Potosi Department, Southern Bolivia
Synchrotron study identifies four major mineralogi cal domains that are within a single
large telescoped porphyry/epithermal mineralizing system
Toronto, Canada, June 25, 2020 – Eloro Resources Lt d. (TSX-V: ELO; FSE: P2Q) (“Eloro”,
or the “Company”) is pleased to announce that its B olivian subsidiary Minera Tupiza SRL has
contracted Empresa Minera Villegas SRL to start underground drill bay preparations required for
the 3,500m underground diamond drilling program pla nned on its Iska Iska Silver-Polymetallic
Project (“Iska Iska”) in the Potosi Department, sou thern Bolivia. The Company and contractor
have implemented safeguards to protect personnel from COVID-19. It is expected that drilling
can commence once Bolivia lifts lockdown restrictio ns. Mineral Tupiza SRL has an option to
acquire a 99% interest in Iska Iska (see press release January 9, 2020).
Preparations will include rehabilitation of 400 meters of underground workings and preparation
of drill bays in the Huayra Kasa mine and in the Mi na 2 underground workings located 2
kilometres south of Huayra Kasa (Figure 1). All wo rkings will be systematically geologically
mapped and channel sampled.
Tom Larsen, President & CEO of Eloro commented: “Th e planned drill program will follow the
outline presented in the National Instrument (“NI”) 43-101 Technical Report by Micon
International Limited (see press release April 29, 2020). This program will be the first drilling to
ever be carried out on the property and is designed to test the full extent of the mineralized system
in the vicinity of the mine workings. Iska Iska is in a prolific district of Bolivia and has excellent
potential to host a significant silver-polymetallic mineral deposit.”
SYNCHROTRON MINERAL STUDY
Eloro contracted Dr. Lisa Van Loon of LISA CAN Analytical Solutions Inc. and Dr. Neil Banerjee
of Western University, Department of Earth Sciences, to carry out a synchrotron mineral cluster
analysis of samples from Iska Iska. The synchrotron is a type of circular particle accelerator that
is an extremely powerful source of broad-spectrum electromagnetic radiation (e.g., visible light,
infrared, UV, & X-rays), approximately 10 billion times brighter than the sun that allows for a rapid,
high-resolution analytical technique for mineral ex ploration. A total of 42 pulps from samples
from the Iska Iska due diligence program (see press release of October 8, 2019) were analysed.
The study concluded that synchrotron mineral cluste r analysis identified four mineralogical
domains that cover the entire sampling area suggesting they are related and represent a single,
large mineralizing system. Furthermore, the minera logy of the domains is consistent with
minerals identified in hand specimen and are likely related to a telescoped porphyry/epithermal
style of mineralization. Domain 1 is the most perv asive being identified in 31 samples while
Domains 2, 3 and 4 are more localized. Table 1 lists the characteristics of each sample domain
with range of assay results and mineralogical data from the synchrotron samples. Table 2 gives
the complete analytical data for all samples analysed in the study.
Dr. Osvaldo Arce, P.Geo., Eloro’s Project Manager in Bolivia, commented: “The results from this
study support the concept of outlining potential bu lk mineable silver-polymetallic mineralization
at Iska Iska as concluded by Micon. Domain 1 is ve ry widespread with mineralization and
alteration occurring in all rock types including granodiorite, dacite and sandstone. Some samples
returned grades comparable to those samples in the more restricted domains. Domain 2 contains
high silver, zinc, lead and indium values while Dom ain 3 has high gold and bismuth values.
Domain 4 returned the highest gold value with high silver and bismuth. It is likely that the
mineralization in Domains 2 to 4 is a precious meta l-rich epithermal style that occurs along
structures cutting the widespread Domain 1 mineralization that is of disseminated porphyry style.
It should be emphasized that this is a preliminary study the conclusions of which will be refined
with additional surface/underground geological mapping and diamond drilling.”
APPOINTMENT OF MICON INTERNATIONAL
Following the completion of the NI 43-101 Technical Report dated April 27, 2020, the next phase
in the development of the Iska Iska polymetallic pr oject is geared towards the preparation of a
maiden mineral resource estimate. To ensure that the highest level of technical and commercial
standards is upheld, Eloro has retained Micon Inter national Limited as Independent Engineer
(“IE”) to review, on an on-going basis, all its exp loration activities and data collection methods.
The IE will also advise on how best to proceed with preliminary metallurgical test-work of which
the results will be critical in the definition of the mineral resources.
QUALIFIED PERSON
Dr. Osvaldo Arce, P. Geo., an expert on Bolivian geology and a Qualified Person in the context
of NI 43-101 has reviewed and approved the technica l content of this news release. Dr. Bill
Pearson, P.Geo., Chief Technical Advisor for Eloro, and who has more than 45 years of
worldwide mining exploration experience including extensive work in South America, will provide
technical oversight to the program in consultation with Eloro’s Technical Advisory Committee and
Micon International.
ABOUT ISKA ISKA
Iska Iska polymetallic project is a road accessible, royalty-free property, wholly-controlled by the
Title Holder, Empresa Minera Villegas S.R.L. and is located 48 km north of Tupiza city, in the
Sud Chichas Province of the Department of Potosi. T he property can be classified as a
polymetallic (Ag, Zn, Pb, Au, Cu, Bi, Sn, In) epithermal-porphyry complex. This is an important
mineral deposit type in Bolivia.
Geological mapping on the property by Eloro has revealed the spatial and temporal zonation of
alteration and vein minerals in an area of about 5 square kilometres. The polymetallic
mineralization occurs mainly as veins, subsidiary v ein swarms, veinlets, stockworks, and
disseminations, forming a subvertical vein system i n both the stock and the volcanic and
sedimentary rocks. Preliminary evaluation work inc luding 42 channel samples in underground
channel samples included altered wall rock with wid ths ranging between 1.20 to 5.55 m,
averaging 2.90 m (see press release of October 8, 2019 for further details).
Silver. Anomalous silver values range between 35.5-694 g/t Ag (46% of channel samples).
Gold. Anomalous gold values range between 0.31-28.6 g/t Au (42% of channel samples).
Zinc. Anomalous zinc values range between 1.05-16.95% Zn (37% of channel samples).
Lead. Anomalous lead values range between 0.41-16.95% Pb (49% of channel samples).
Copper. Anomalous copper values range between 0.1->1% (22% of channel samples).
Bismuth. Anomalous bismuth values range between 967-7,380 g/ t Bi (22% of channel
samples).
Indium. Anomalous indium values range between 10.35->500 g/ t In (34% of channel
samples).
ABOUT ELORO RESOURCES LTD.
Eloro is an exploration and mine development company with a portfolio of gold and base-metal
properties in Bolivia, Peru and Quebec. Eloro has an option to acquire a 99% interest in the highly
prospective Iska Iska Property, which can be classi fied as a polymetallic epithermal-porphyry
complex, a significant mineral deposit type in the Potosi Department, in southern Bolivia. Eloro
recently commissioned a NI 43-101 Technical Report on Iska Iska, which was completed by
Micon International Limited and is available on Eloro’s website and under its filings on SEDAR.
Iska Iska is a road-accessible, royalty-free property. Eloro also owns an 82% interest in the La
Victoria Gold/Silver Project, located in the North-Central Mineral Belt of Peru some 50 km south
of Barrick’s Lagunas Norte Gold Mine and Pan American Silver’s La Arena Gold Mine. La Victoria
consists of eight mining concessions and eight mini ng claims encompassing approximately 89
square kilometres. La Victoria has good infrastructure with access to road, water and electricity
and is located at an altitude that ranges from 3,150 m to 4,400 m above sea level.
CAUTION REGARDING FORWARD-LOOKING INFORMATION
Information in this news release may contain forward-looking information. Statements containing
forward looking information express, as at the date of this news release, the Company’s plans,
estimates, forecasts, projections, expectations, or beliefs as to future events or results and are
believed to be reasonable based on information currently available to the Company. There can
be no assurance that statements of forward-looking information will prove to be accurate. Actual
results and future events could differ materially f rom those anticipated in such statements.
Readers should not place undue reliance on forward-looking information.
Neither the TSXV nor its Regulation Services Provider (as that term is defined in the policies of
the TSXV) accepts responsibility for the adequacy or accuracy of this release.
FOR FURTHER INFORMATION PLEASE CONTACT:
Thomas G. Larsen (President & CEO) Jorge Estepa (Vi ce-President)
[email protected] [email protected]
ELORO RESOURCES LTD
20 Adelaide Street East, Suite 200 PHONE (416) 868-9168 | FAX (416) 361-1333
Toronto, Ontario, Canada M5C 2T6 www.elororesources.com
FIGURE 1: LOCATION MAP AND PLAN MAP OF UNDERGROUND WORKINGS AT HUAYRA KASA SHOWING LOCATION OF
DOMAINS DEFINED IN SYNCHROTRON STUDY
TABLE 1: SYNCHROTON MINERALOGICAL ANALYSIS
py = pyrite; mc = marcasite; sph = sphalerite; gn = galena; apy = arsenopyrite; sd = siderite; agt = argentite; spls = samples ; n.d. = not detected
Domain
No.
Spls
Grade Range of Main Metals
Main Minerals
Characteristics
Au g/t Ag g/t Zn% Pb% Bi
ppm
In
ppm
Cu % Sn % Py Mc Sph Gn Apy Sd Agt
1
31
0.32-
15.50
(39%
of total
spls)
8.99 -
362
(48% of
total
spls)
0.3-
2.15
(51.6%
of total
spls)
0.25-
9.53
(51.6
% of
total
spls)
23.7-
5,860
(67.7%
of total
spls)
4.72-
˃500
(˃64.5
% of
total
spls)
0.02-˃1
(74.1%
of total
spls)
0.01-
˃0.05
(51.6%
of total
spls)
major
major
major
major
n.d.
minor
n.d.
Quartz,
muscovite,
sulphides
(pyrite), low gold,
low silver, high
bismuth and low
indium
2
5
0.02-
0.35
(40%
of total
spls)
204-694
(100%
of total
spls)
0.39-
16.95
(100%
of total
spls)
0.15-
16.95
(100
% of
total
spls)
30.70-
73
(80% of
total
spls)
46.40-
˃500
(100%
of total
spls)
0.05-
0.15
(74.1%
of total
spls)
<0.01%
(100%
of total
spls)
major
n.d.
major
major
n.d.
minor
trace
Galena, pyrite,
quartz,
muscovite, low
gold, high silver,
zinc, lead and
highest indium.
High correlation
silver and indium
3
3
2.18-
9.10
(100%
of total
spls)
68.90-
295
(100%
of total
spls)
3.75-
3.80
(66.6%
of total
spls)
0.48-
3.75
(100
% of
total
spls)
334-
3160
(100%
of total
spls)
5.44-
323
(100%
of total
spls)
0.05˃1
(100%
of total
spls)
0.01-
˃0.05
(100%
of total
spls)
major
major
major
major
minor
minor
trace
Sulphides
(pyrite), quartz,
high gold,
moderate silver,
high bismuth.
High correlation
gold and bismuth
4
1
28.60
61.60
0.01
0.41
7,380
4.37
0.31
<0.01%
minor
major
n.d.
n.d.
n.d.
n.d.
n.d.
Scorodite,
tourmaline
dravite, quartz,
highest gold,
high silver,
highest bismuth
and low indium
TABLE 2: DETAILED ANALYTICAL DATA BY DOMAIN FOR SAMPLES ANALYZED IN THE SYNCHROTRON STUDY
Domain Sample No. Au g/t Ag g/t Zn % Pb % Cu % Bi ppm In p pm Sn ppm
1
HK 01 0.01 0.53 0.01 0.01 0.02 12.50 1.08 44.90
HK 02 0.36 1.39 0.51 0.44 0.05 123 4.72 57.80
HK 03 2.50 25.50 2.15 0.63 0.06 967 9.76 108
HK 04 0.85 10.50 1.99 0.28 0.04 52.50 26.3 71.70
HK 06 0.07 46.10 3.01 0.77 0.05 40.80 ˃500 77.60
HK 08 0.02 75.10 1.40 1.35 0.02 40.40 102 65.60
HK 11 <0.01 1.67 0.69 0.15 0.01 23.70 9.68 36.60
HK 12 <0.01 3.78 1.29 0.8 0.01 194 5.67 81.40
HK 13 <0.01 3.10 0.39 0.15 0.01 1.25 9.55 66.80
HK 14 0.04 13.60 0.38 0.43 0.02 4.12 2.82 52.10
HK 15 <0.01 1.82 1.05 0.03 0.01 1.81 2.07 66.80
HK 16 <0.01 0.85 0.08 0.01 0.01 2.02 0.99 38.70
HK 17 <0.01 5.99 0.31 0.25 0.01 3.06 1.83 105
HK 19 0.03 37.70 1.51 1.33 0.04 44.10 8.95 ˃500
HK 21 0.34 2.60 0.51 0.07 0.02 101 3.95 25
HK 23 12.4 57.4 1.86 1.44 0.02 1,200 19.40 42
HK 24 0.03 3.030 0.01 0.21 0.04 36.70 7.09 185
HK 25 0.32 26.90 0.01 1.16 0.04 163 28.50 ˃500
HK 27 1.61 55.70 0.01 0.11 ˃1.00 503 4.78 ˃500
HK 28 1.65 321 0.01 0.35 0.29 1,850 16.90 ˃500
HK 29 0.60 68.70 0.01 0.01 ˃1.00 1,500 10.40 ˃500
HK 30 0.01 1.72 0.01 0.00 0.01 6.31 0.50 128
HK 31 2.60 288 0.01 0.42 0.14 2,850 10.60 ˃500
HK 32 0.02 2.90 0.02 0.01 0.14 21.04 0.83 75.40
HK 33 0.11 4.06 0.02 0.17 0.10 18.40 5.21 40.40
HK 34 0.02 1.61 0.01 0.01 0.01 17.70 0.69 59
HK 35 0.01 0.55 0.01 0.01 0.01 6.17 0.58 43.60
HK 36 2.14 8.99 0.01 0.72 0.02 646 5.84 30.90
HK 37 0.08 1.43 0.01 0.07 0.01 8.97 3.88 90
HK 39 0.15 1.15 0.01 0.01 0.01 42.10 1.13 65.50
HK 41 0.19 73.4 5.63 1.08 0.03 48 32.2 172
2
HK 07 0.35 204 4.81 4.13 0.05 30.70 384 283
HK 09 0.02 266 5.75 8.24 0.01 71 46.40 248
HK 10 0.01 570 10.60 9.72 0.15 73 ˃500 136
HK 18 0.03 362 9.23 9.53 0.03 66.80 23 845
HK 42 0.01 694 7.87 16.95 0.06 37 ˃500 182
3
HK 22 9.10 73.70 3.80 1.70 0.08 1,230 323 30.1
HK 26 2.71 295 0.02 0.48 ˃1.0 3,160 24.10 ˃500
HK 40 2.18 68.90 3.75 3.75 0.05 334 5.44 311
4 HK 38 28.60 61.60 0.01 0.41 0.31 7,380 4.37 17