www.cypriummining.com
TSX-V: CUG and CUG.DB
MONTREAL, July 20, 2016 /CNW Telbec/ - Cyprium Mining
Corporation ("Cyprium" or the "Company") (TSXV: CUG
CUG.DB) is pleased to announce the results from 71 additional
underground samples taken from the Tunel body as part of its ongoing exploration
program of the Potosi silver mine
located in Santa Eulalia, Mexico.
Of the 71 samples taken, 34 were channel samples taken at the
edges of old stopes on levels 1 and 2, and 37 samples were of
previously broken mineralized rock from levels 1, 2 and 3 that was
left behind at the end of the last mining in this area. All
samples were taken in areas where Cyprium expects initial
production to take place (1).
The 34 channel samples were taken on exposures of relatively
flat lying manto and steep chimney mineralization on levels 1 and
2. Not including eight samples of oxidized mineralization from a
chimney on level 2, 26 samples averaged 238g/t Ag, 5.28% lead, and
8.04% zinc over an average sample width of 1.2 m. The table below
shows averages for sampling on different levels of the Tunel body, including some previously reported
sampling from levels 3 and 4 (see press release of June 9, 2016 and June
13, 2016). All of these exposures are at the margins
of historic workings near the Potosi No. 3 shaft. The shaft has
been reconditioned with a haulage system capable of removing
approximately 100 tons per day (1) and compressed air
and water have been brought in, with an air compressor installed on
Level 2.
Previously broken rock, termed 'muck' or in Spanish, 'rezaga'
was left behind in old stopes and mineralized material passes in
several places within the Tunel
body. This material has been moved down to the haulage level (level
2) to be removed from the mine via the recently rehabilitated and
now operational shaft No. 3. The assays from this material average
173 g/t silver, 4.8% lead and 3.9% zinc for an average sample
weight of 6.1 kg and a total of 224 kg. It is estimated that enough
tonnage of this material is ready to be removed from the mine to
conduct the initial extraction tests, ahead of the Company's
expected explosive permit grant.
Area
|
Samples
|
Width
m
|
Au
g/t
|
Ag
g/t
|
Pb%
|
Zn
%
|
Level 1
manto
|
9
|
0.9
|
-
|
317
|
6.34
|
10.08
|
Level 1
chimney
|
11
|
1.4
|
-
|
196
|
4.48
|
7.15
|
Level 2
manto
|
6
|
1.1
|
-
|
243
|
5.87
|
7.65
|
Level
3½*
|
13
|
1.5
|
0.074
|
206
|
6.40
|
5.99
|
Level 4 manto Zone
A**
|
18
|
1.4
|
-
|
194
|
0.78
|
0.58
|
Level 4 manto Zone
B**
|
19
|
1.4
|
-
|
192
|
1.12
|
0.61
|
Level 4 high grade
vein
|
6
|
1.0
|
0.295
|
646
|
6.35
|
2.87
|
* Some samples from
this interval were previously included in the news releases of June
13, 2016.
|
** Selected samples
as previously reported in the news release of June 9,
2013.
|
The results announced today are part of an ongoing exploration
program to evaluate the potential of known mineralization in the
Tunel body near the Potosi No. 3
shaft. This shaft has been rehabilitated and provides access for
services such as compressed air and for haulage of broken
mineralized rock from the Tunel
body on levels 2 to 4 (see News Releases of June 9 and Jun13, 2016) where underground
exploration and development will begin shortly. Work is also in
progress for the Santo Domingo
body, also known as Main Silicate body, which was also partly mined
in the past at levels 9 to 11. Efforts are underway to determine
the volume and grades of remaining material in this area, which is
not accessed by the Potosi No. 3 shaft. Past production from the
Santo Domingo body was from the
Potosi No. 1 and Potosi No. 5 shafts and from a shaft on
neighboring ground controlled by a third-party. Plans for gaining
access to the Santo Domingo body
are currently in consideration.
Mineralization in the area where the samples were taken is
exposed in a large chimney that extends over several levels.
Although most of the mineralization on the upper levels of the
Potosi mine is oxidized, local
areas with preserved sulfides on the upper levels were discovered
in the last few decades (2). The main exposures of
sulfide mineralization studied to date are on levels 9 to 11, but
the sulfide material also extends upward to level 6. Such sulfide
orebodies were not economically exploitable prior to the advent of
selective flotation in the early 1900's and were evidently left
behind for this reason and later forgotten. These "perched" sulfide
bodies were possibly preserved due to the vagaries of past
oxidation.
The Santa Eulalia
District
Santa Eulalia is a world class
polymetallic mining district located in the central part of the
State of Chihuahua, Mexico,
approximately twenty-two kilometers east of the City of Chihuahua.
Mineralization in the area was originally discovered during the
Spanish colonial period in the 1500's, and recorded production has
occurred over more than 300 years. Santa
Eulalia ranks as one of Mexico's primary silver and base metal
producing districts with nearly 450 million ounces of silver and
substantial amounts of lead and zinc mined. The nature of the
deposit in the Santa Eulalia
district is a carbonate replacement deposit and is the historically
largest of its type in Mexico.
Mineralization occurs in an area about 10 km in length and 5 km in
width. Production and reserves for the district have been
estimated to be about 50 million metric tons (3) with
grades of 125-350 g/t Ag, 2-8% Pb and 3-12% Zn (3) (4),
along with appreciable quantities of tin and vanadium.
The Santa Eulalia district
covers approximately forty-eight square kilometers and is divided
into three areas, the West Camp, the Central Camp and the East
Camp. The Potosi silver mine is
located in the West Camp. The West Camp has produced most of the
minerals from the district from an area 4 km long in a north-south
direction and 2 km wide in an east-west direction, with the
Potosi silver mine being one of
the primary producers.
Based on the geology, past mining activity and the exploration
work completed by the Company to date, the Potosi mine, the Company believes that the
project warrants further exploration. Widely spaced sampling on
levels 2 to 4 in the area of the Potosi No. 3 shaft (Tunel body) and levels 6 and 9-11 in the area
of the Potosi No.1 shaft (Santo
Domingo or Main Silicate body) has shown that mineralized
material of interesting grades is exposed at the margins old stopes
and adjacent areas, and this work will continue in order to
evaluate the potential for defining resources.
Geological Setting, Deposit Type and Mineralization
Mineralization in the Santa
Eulalia district is characterized by massive sulfides,
dominantly pyrrhotite, sphalerite, galena and pyrite that are
hosted mainly in horizontal mantos and steep chimneys of sulfide
material that replace limestone, with some breccia bodies also
occurring. Mineralized bodies occur along laterally
continuous discrete structural zones that mainly trend in a
north-south orientation, with mineralization forming preferentially
in certain stratigraphic units. Past mining has reached to as
much as 700 meters depth below the surface on 21 levels.
Production in the West camp was diminished until the late 80's with
the discovery of new mineralization. Currently there is little
production in the district.
National Policy 43-101 Report
Cyprium has engaged Dr. Craig
Gibson to complete a National Instrument 43-101 report with
respect to the initial mine levels 2, 3 and 4 of the Potosi silver mine. It is expected the report
will be completed before the end of June
2016. The report to be prepared by Dr. Gibson shall not
contain a resource or reserve calculation.
Quality Assurance and Control
Samples taken in underground workings are typically channel
samples. Sample cuttings consist of rock chips taken along
pre-marked channels approximately 15-20 cm in width that span the
mineralized zone and are collected at the site by an experienced
sampling crew under the supervision of a Company geologist.
Sample material generally consists of from 2.0 to more than 4.5 kg
of material that is placed in labelled plastic bags that are sealed
with ties at the collection site. Samples taken of the broken
rock ranged from 2.35 to 11.27 kg and were taken from various areas
of the volume of rock. The samples were transported from the
mine and stored at the Company's or contractor's surface facilities
and subsequently taken directly to the lab preparation
facility. The samples are transported in Company vehicles and
delivered to the sample preparation facility by personnel of the
company or contractor.
All samples were analyzed in Vancouver for the reported metals by the
ME-OG62 method for higher grade samples. Internal control
samples were added to the sample stream every 20th
sample and the laboratory applies strict quality control
procedures. ALS Chemex is part of ALS Global, an
internationally recognized analytical laboratory.
Neither 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.
Qualified Person: Dr. Craig
Gibson, Certified Professional Geologist, prepared the
summary of public historical information on the Santa Eulalia district, and has reviewed the
appropriate portions of this news release and approved the contents
thereof. Public information included in this release are
based on work by from a PhD dissertation by Peter K. M. Megaw and information from the
Mexican Geologcial Survey (Servicio Geologico Mexicano).
References:
(1) See important disclaimer in bold below.
(2) P. Megaw, pers. Comm.
(3) Megaw, P.K.M., 1990, Geology and geochemistry of the
Santa Eulalia mining district,
Chihuahua, Mexico, unpublished PhD
dissertation, University of Arizona,
461 pp.
(4) Bustos-Diaz, J.L. and Arzabala-Molina, J., 2007,
Monografia Geologico-Minera del Estado de Chihuahua, Servicio
Geologico Mexicano, 640pp.
This news release contains "forward-looking information"
(within the meaning of applicable Canadian securities laws) and
"forward -looking statements" (within the meaning of the U.S.
Private Securities Litigation Reform Act of 1995). Such statements
or information are identified with words such as "anticipate",
"believe", "expect", "plan", "intend", "potential", "estimate",
"propose", "project", "outlook", "foresee" or similar words
suggesting future outcomes or statements regarding an outlook. Such
statements include, among others, those concerning the Company's
anticipated plans for developments of the Company and its mining
projects".
Such forward-looking information or statements are based on a
number of risks, uncertainties and assumptions which may cause
actual results or other expectations to differ materially from
those anticipated and which may prove to be incorrect. Assumptions
have been made regarding, among other things, management's
expectations regarding future growth, plans for and completion of
projects by Company's third party relationships, availability of
capital, and the necessity to incur capital and other expenditures.
Actual results could differ materially due to a number of factors,
including, without limitation, operational risks in the completion
of Company's anticipated projects, delays or changes in plans with
respect to the development of Company's anticipated projects by
Company's third party relationships, risks affecting the ability to
develop projects, risks inherent in operating in foreign
jurisdictions, the ability to attract key personnel, and the
inability to raise additional capital. No assurances can be given
that the efforts by the Company will be successful. Additional
assumptions and risks are set out in detail in the Company's
MD&A, available on SEDAR at
www.sedar.com.
Although the Company believes that the expectations reflected
in the forward-looking information or statements are reasonable,
prospective investors in the Company's securities should not place
undue reliance on forward-looking statements because the Company
can provide no assurance that such expectations will prove to be
correct. Forward-looking information and statements contained in
this news release are as of the date of this news release and the
Company assumes no obligation to update or revise this
forward-looking information and statements except as required by
law.
Investors should note that the Potosi silver mine and La Chinche property
have no established mineral resources or mineral reserves as
defined by NI 43-101. Although Cyprium Mining has made a production
decision regarding the Potosi
silver mine based on historical production records and results from
recent sampling, a feasibility study of its projects has not been
completed and there is no certainty that the proposed operations
will be economically or technically viable. It must be understood
that any such production would be from unmeasured mineralized
material. The Company further advises that since its
production decision was not based on a feasibility study of mineral
reserves demonstrating economic and technical viability there may
be an increased uncertainty of achieving any particular level of
recovery of minerals or the cost of such recovery, including
increased risks associated with developing a commercially mineable
deposit. Historically, such projects have a much higher risk of
economic and technical failure. These risks, among others, include
areas that are analysed in more detail in a feasibility study, such
as applying economic analysis to resources and reserves, more
detailed metallurgy and a number of specialized studies in areas
such as mining and recovery methods, market analysis, and
environmental and community impacts. There is no guarantee that
production will proceed as anticipated or at all or that
anticipated production costs will be achieved. Failure of
production to proceed as planned would have a material adverse
impact on the Company's ability to generate revenue and cash flow
to fund operations. Failure to achieve the anticipated production
costs would have a material adverse impact on the Company's cash
flow and future profitability.
SOURCE Cyprium Mining Corporation