VANCOUVER, Aug. 19, 2014 /CNW/ - Mundoro Capital Inc. (TSXV: MUN, www.mundoro.com) ("Mundoro" or the "Company") is pleased to announce drilling results
from its Tilva Rosh prospect within the Savinac exploration license in
northeastern Serbia. The Savinac license covers 90 km2 and is located within the Timok Magmatic Belt, approximately 20 km
southeast of the Bor mining camp.
Teo Dechev, CEO and President of Mundoro commented, "This initial
drilling program at Tilva Rosh was designed to test step-out extensions
of the mineralization down dip and along strike. The initial drilling
results have successfully demonstrated continuation of surface
mineralisation at depth, along strike and are encouraging as management
believes the results are vectoring towards a deeper mineralisation
source. The mineralization is open to the north, south and at depth."
Six inclined diamond drill holes totaling 917.8 m were drilled at the
southern portion of Tilva Rosh system to test the vertical extent of
the gold mineralization, which was previously confirmed by high grade
trenching results of 12 m @ 33.03 g/t AuEq (30.39 g/t Au, 171.27 g/t
Ag) (see October 21, 2013 press release). The drill holes were designed
to test the down dip mineralization to a maximum of 150 m down dip.
Collar locations are shown on Figure 1 -Tilva Rosh Drill Plan. Cross section of interpreted geology shown in Figure 2 - Tilva Rosh - Cross Section A-A'.
Table 1: Summary of significant results from drill holes SAV01 to SAV06.
Drill Hole ID
|
From
(m)
|
To
(m)
|
Interval
(m)
|
Au (g/t)
|
Cu (%)
|
Ag (g/t)
|
AuEq
(g/t)
|
CuEq
(%)
|
SAV_01
Including
Including
|
11
|
18
|
7
|
7.90
|
_
|
46.74
|
8.68
|
_
|
13
|
15
|
2
|
24.98
|
_
|
128.05
|
21.11
|
_
|
13
|
14
|
1
|
42.90
|
_
|
199
|
46.22
|
_
|
126
|
133
|
7
|
0.35
|
_
|
2.76
|
0.40
|
|
SAV_02
|
30
|
40
|
10
|
0.34
|
_
|
2.16
|
0.38
|
_
|
67.7
|
71.8
|
4.1
|
0.62
|
_
|
2.36
|
0.66
|
_
|
95.6
|
100.0
|
4.4
|
0.54
|
_
|
6.38
|
0.65
|
_
|
SAV_03
Including
|
71.0
|
76.0
|
5.0
|
2.54
|
0.59
|
15.54
|
3.73
|
2.36
|
74.0
|
74.7
|
0.7
|
10.35
|
1.47
|
50.10
|
13.52
|
8.54
|
SAV_04
Including
|
42.2
|
51.3
|
9.1
|
1.24
|
0.33
|
9.00
|
1.91
|
1.21
|
43.3
|
47.3
|
3.0
|
1.45
|
0.58
|
14.60
|
2.61
|
1.65
|
SAV_05
Including
Including
|
29
|
50.2
|
21.2
|
0.25
|
_
|
1.78
|
0.28
|
_
|
30.4
|
36.0
|
5.6
|
0.43
|
_
|
3.30
|
0.49
|
_
|
46.2
|
50.2
|
4.0
|
0.35
|
0.14
|
3.88
|
0.63
|
0.40
|
SAV_06
|
38.50
|
42.90
|
4.4
|
0.59
|
0.21
|
14.95
|
1.17
|
0.74
|
Gold Equivalent ("AuEq.") is calculated using the formula AuEq =
(g/t/Au) + (g/t/Ag) + ($/ozAu)/65 + [(%Cu) x (22.0462) x ($/lbCu)] ÷
[(1/31.1035) x ($/ozAu)]. Copper equivalent (CuEq%) is calculated using
the formula CuEq = (%Cu) + [(g/t/AuEq) x (1/31.1035) x ($/ozAu)] ÷
[(22.0462) x ($/lbCu)]. Metal prices used are: gold price of
US$1300/oz, copper price of US$3/lb, and silver price US$20/oz. All thicknesses from intersections from drill holes are down-hole
drilled thicknesses or outcrop sample length thickness.
The Tilva Rosh drilling program has demonstrated continuation of surface
mineralisation at depth and along strike of a north-west structure
responsible for the high grade gold. The Au-Ag mineralization
identified in the in-soil geochemistry anomaly and confirmed in the
trenching, has now been confirmed at a depth to 76m, along strike for
100 m (50 m to south and 50 m to north) and remains open in all
directions. Copper mineralisation was intersected at depth in four of
the six drill holes (SAV03-SAV06). Management believes copper was not
present at surface due to the highly acidic nature of the lithocap in
the area caused by the high pyrite content in the system. The eastern
most drill holes, SAV02 and SAV05, intersected the highest lead-zinc
contents (up to 2.2 % Zn and 0.6 % Pb) suggesting lateral zoning
indicative of porphyry style hydrothermal system.
These initial drill results at Tilva Rosh are encouraging and are
interpreted to be proximal to a Cu-Au porphyry system related to a
large area of advanced argillic lithocaps to the north, highlighted
with a central Mo anomaly rimmed by Cu and followed outwards to zones
of Pb-Zn. This is classic geochemical signatures of porphyry deposit
footprints and where the company believes exist further porphyry drill
targets.
Drill Hole Highlights of Tilva Rosh Prospect
Over the past 18 months Mundoro has conducted geochemical, mapping,
trenching, ground magnetic surveys over this license as well as
compiling historic data, targeting epithermal and porphyry Cu-Au
systems. This work has outlined the Savinac mineralised belt (9 km by 2
km) which includes the Tilva Rosh epithermal system expressed on the
surface with a large area of advanced argillic alteration covering 4km
by 1km. Tilva Rosh prospect was explored previously in late 1970's and
early 2000's but significant gold mineralisation and porphyry Cu-Au
potential was identified by Mundoro's exploration in Q4-2013.
SAV 01 intersected a hydrothermal breccia and veinlet zone similar to the
out-cropping high grade (69.7 m). At 102.3m the hole cut argillic
altered feldspar andesite porphyry with quartz veinlets and pyrite
content 2-5% throughout and minor chalcopyrite mineralisation at
150.9m.
SAV 02 intersected 8.5 meters of iron oxide breccia with silicified clasts and
continued in a hydrothermal breccia with pyrite down to 40.3 m. As in
SAV 01, it then cut andesite feldspar porphyry from 30.9 m to the end
of the hole (158.7 m). SAV 02 is characterized by more faulting and
veining of the andesite porphyry and sphalerite-galena mineralisation
in the quartz veins.
SAV 03 collared in a quartz-iron oxide hydrothermal breccia which continued
down to 48.7 m. From 52.5 m to 82.6 m the drill hole intersected a
fault zone which contains semi-massive pyrite chalcopyrite-chalcocite
mineralisation from 69.9 m to 74.7 m (4.8 m). A-type porphyry veins
were noted from 115.6 m to 121 m (5.4 m) passing to gypsum/anhydrite
stockwork veining and quartz-pyrite veinlets to the end of the hole.
SAV 04 collared in hydrothermal breccia and intersected quartz-pyrite in
andesite and lithic tuff which is moderately argillic altered with rare
pyrite±chalcopyrite veinlets (from 23.8 m to 29.8 m). From 41.3 m, the
drill hole intersected fault breccia with quartz-massive
pyrite-sphalerite ± galena veins containing up to 30% pyrite. From 52.4
m the drill hole intersected andesite feldspar porphyry, cross cut by
quartz-pyrite vein and veinlets, vuggy texture
quartz-pyrite-sphalerite±galena vein with massive pyrite up to 15%) and
a hydrothermal breccia zones with quartz-pyrite veins.
SAV 05 collared in argillic altered andesite porphyry with quartz veinlets
with disseminated pyrite and pyrite in fracture fills 1-3% continuing
to the end of hole (149.7 m). From 19.3 m to 94.5 m the drillhole cut
through a fault and quartz vein zone containing irregular
pyrite-barite-sphalerite galena mineralisation.
SAV 06 is the shortest hole drilled (116.3 m). It cut quartz-hydrothermal
breccia from 0 m to 8.6 m hosted in lithic tuff and continued in
andesitic tuff with ~1% pyrite to 38.6 m. From 38.6 m to 67.2 m it
entered a fault zone containing quartz veins with 1-2% pyrite and
finished in silicified and brecciated andesite containing pyrite and
anhydrite veining.
Sampling, Analysis and Qualified Person
Drill hole orientations were surveyed at approximately 50 meters
intervals. Drill core was collected from drill sites by the Company's
geologists and processed and sampled at the Company's core shed
according to industry best practice standard procedures. Samples were
collected as half PQ or HQ core at one meter lengths from mineralised
intervals and two meter lengths from none mineralised intervals. Where
necessary the sampling lengths were adjusted to reflect the geological
boundaries.
All samples are assayed using 50 gram fire assay with atomic absorption
finish and ME-ICP61 by ALS Romania. The entire sample was crushed to
2mm, then split off a 1 kg sample and pulverized the split to better
than 85% passing 75 microns. Quality Assurance and Quality Control
procedures include the systematic insertion of standards and duplicates
into the sample streams. Duplicate core samples are taken every 25
samples and standards and blanks are inserted after every 20th sample.
All data collected from detailed logging and assay results from the
laboratories are routinely verified and entered in an Access data base.
Technical information contained in this Press Release has been reviewed
and approved by Mr. G. Magaranov, P. Geo., Qualified Person as defined
by National Instrument 43-101.
On behalf of the Company,
Teo Dechev, Chief Executive Officer, President and Director
About Mundoro Capital Inc.
Mundoro is a well-funded, Canadian based, company focused on mineral
acquisition, exploration, and development. Our primary focus is
advancing our properties on the Tethyan Belt in Southeastern Europe.
Mundoro has methodically acquired a district-scale land position on
this prolific mineral belt which hosts significant Gold-Copper porphyry
and related epithermal deposits. Our strong project pipeline, which
also includes assets in Mexico and China, is positioned to drive
long-term, sustainable growth in order to attain production and
shareholder return.
Caution Concerning Forward-Looking Statements
Information included, attached to or incorporated by reference into this
News Release may contain forward-looking statements. All statements,
other than statements of historical fact, included or incorporated by
reference in this News Release are forward-looking statements,
including, without limitation, statements regarding activities, events
or developments that the Board expects or anticipates may occur in the
future. These forward-looking statements can be identified by the use
of forward-looking words such as "will", "expect", "intend", "plan",
"estimate", "anticipate", "believe" or "continue" or similar words or
the negative thereof. The material assumptions that were applied in
making the forward looking statements in this News Release include
expectations as to the Company's future strategy and business plan and
execution of the Company's existing plans. There can be no assurance
that the plans, intentions or expectations upon which these
forward-looking statements are based will occur. We caution readers of
this News Release not to place undue reliance on forward looking
statements contained in this News Release, which are not a guarantee of
performance and are subject to a number of uncertainties and other
factors that could cause actual results to differ materially from those
expressed or implied by such forward-looking statements. These factors
include general economic and market conditions, changes in law,
regulatory processes, the status of Mundoro's assets and financial
condition, actions of competitors and the ability to implement business
strategies and pursue business opportunities. The forward-looking
statements contained in this News Release are expressly qualified in
their entirety by this cautionary statement. The forward-looking
statements included in this News Release are made as of the date of
this News Release and the Board undertakes no obligation to publicly
update such forward-looking statements to reflect new information,
subsequent events or otherwise, except as required by law. Shareholders
are cautioned that all forward-looking statements involve risks and
uncertainties and for a more detailed discussion of such risks and
other factors that could cause actual results to differ materially from
those expressed or implied by such forward-looking statements, refer to
the Company's filings with the Canadian securities regulators available
on www.sedar.com.
Neither 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 release.
SOURCE Mundoro Capital Inc.
For further information please contact Teo Dechev, CEO, President and Director of Mundoro Capital Inc. at +1-604-669-8055 or Michelle Roth, Roth Investor Relations at +1-732-792-2200.