Chesapeake Gold Corp. (“Chesapeake”) (TSX-V:CKG) is pleased to
provide an update of the Phase 1 drilling and district wide
exploration program at its regional Yarely project (“Yarely”) in
Sinaloa State, Mexico. Yarely is strategically located 10
kilometres from a paved highway and within 25 kilometres of the
proposed Metates processing plant site. Metates hosts one of the
largest undeveloped gold, silver and zinc reserves in the world and
is 100% owned by Chesapeake.
During the past year, Chesapeake has assembled a
land position of 72,000 contiguous hectares at Yarely. In 2017, a
systematic exploration program has been undertaken including
geological mapping, rock chip channel sampling and trenching
supplemented by an extensive IP/Resistivity geophysics survey. The
exploration work has led to the discovery of precious and base
metal mineralization hosted within several different deposit types
including skarns, veins, disseminated zones, stockwork and
breccias. Six separate significant prospects have been defined
namely: Central, Loretos, Yasmin, Lucy, Sundae and Los Mimbres.
The Phase I 5,000 metre drill program commenced
in October. The first drill holes were designed to test the Central
Prospect’s large IP anomalies and the Spaniards vein swarm. To
date, five core holes totaling 1,200 metres have been completed in
the Central Prospect (see attached map and table).
http://resource.globenewswire.com/Resource/Download/99ab24d8-1d4d-4d5a-b3c9-c08ee609bd7c
http://resource.globenewswire.com/Resource/Download/b2f2366f-54bb-497b-bfee-5c4f6bc377da
Central Prospect
The Central Prospect’s southern area hosts four
subparallel north-northwest trending stockwork zones over one
kilometre in length. These structural corridors bracket a strong
northeast trending IP chargeability anomaly several kilometres long
and one kilometre wide. Two widely spaced exploratory holes (Y-02
and Y-03) were designed to provide data on the thickness of the
stratigraphic units overlying a possible intrusive, the vertical
geochemical and rock alterations zonation, the size and shape of
potential mineralized bodies, and to determine the mineralogical
nature of the IP anomaly. Holes Y-02 and Y-03 were spaced 650
metres apart and are outlined below:
- Drill hole Y-02 was drilled to intersect the IP chargeability
anomaly at less than 300 metres depth. The hole intersected highly
altered sandstone, conglomerate and minor siltstone, which have
locally converted to hornfels. The bottom 189 metres of the hole
contained variable disseminated pyrite and veinlets with trace
chalcopyrite and averaged 421 ppm copper, suggesting the existence
of a copper-mineralized intrusive system.
- Drill hole Y-03 was drilled to intersect a northeast-trending
breccia zone and the adjacent IP anomaly. Similar to Y-02, the hole
from top to bottom intersected a highly altered sedimentary
package. Two intervals including 45 metres (19 to 64 metres) of 2.5
g/t silver and 0.30% zinc and 45 metres (250 to 295 metres) of 3.0
g/t silver and 432 ppm copper demonstrate a zonation of shallow
zinc to copper at depth similar to Y-02.
Drill hole Y-01 was collared 800 metres
southwest of Y-02 and targeted a northwest-trending stockwork
quartz zone outside the high IP anomaly. The hole intersected 17
metres of anomalous gold and silver values in altered sandstone
with disseminated pyrite. Y-01 did not cut the quartz veining
sampled on surface (25 metres of 0.9 g/t gold and 24 g/t silver)
due to a change in dip orientation.
Central - Spaniard Zone
The Spaniard zone is located in the northern
part of the Central Prospect and contains a swarm of
north-northeast trending quartz-calcite veins with oxidized gold
and silver mineralization. The veins average 2 metres in width and
can be traced for over a kilometre in length. During the Spanish
Colonial period, the oxidized veins were mined to an average depth
of 15 metres before encountering transitional sulfides. The drill
program is targeting the lateral and down dip mineralized
continuity of these sulfide bearing veins. Two holes, Y-05
and Y-06, drilled the same vein at different depths along the same
section.
- Drill hole Y-05 was drilled to cut the vein at a shallow depth.
The single vein was intersected at 42 metres downhole where a 1.0
metre intercept returned 6.3 g/t gold, 969 g/t silver, 0.5% lead,
0.6% zinc.
- Drill hole Y-06 was drilled to cut the vein at an intermediate
depth. The faulted vein was intersected at 70 metres downhole where
a 5.1 metre drill sample assayed 0.6 g/t gold and 58 g/t
silver.
Results from holes Y-05 and Y-06 confirm that
sulfide precious metal mineralization likely extends to at least
100 metres depth. To date, ten veins have been discovered and
traced within the swarm encompassing 1,000 metres in width and
1,500 metres along strike.
Loretos Prospect
Loretos is located west of the Central Prospect.
Hole Y-04 is collared 1,500 metres west of hole Y-02 adjacent to a
separate high IP anomaly. Altered and mineralized limestone
outcrops suggest the existence of an intrusive body that generated
widespread hydrothermal activity. A second diamond drill rig was
added in late November. The drill rig experienced mechanical
problems delaying hole Y-04 progress. Currently, Y-04 is advancing
below 300 metres depth and has intersected over 100 metres of
potassic feldspar and silica flooded breccias cut by quartz
veinlets with associated sulfides. The targets are skarns, breccia
bodies and a proximal mineralized intrusive.
Yasmin Prospect
Yasmin is a large quartz vein system related to
a breccia body. During 2017, Chesapeake completed 40 kilometres of
IP survey lines and 4 kilometres of mechanized trenching. At least
two strong chargeability anomalies have been defined one of which
is more than 4 kilometres along strike and up to 900 metres wide.
Geochemical sampling from a trench over the anomaly returned values
from 0.1 to 0.7 g/t gold in zones 5 to 30 metres wide. Quartz veins
samples further to the northeast yielded 3.3 metres of 5.0 g/t
gold, 179 g/t silver and 3 metres of 4.2 g/t gold.
Lucy Prospect
At Lucy, polymetallic carbonate replacement and
multiple mantos are hosted within limestones. Recent exploration
traced this non-continuous zone over 1.5 kilometres along strike.
Channel sampling returned 30 metres of 0.4 g/t gold, 12 g/t silver,
and 3.7% zinc and 3 metres of 0.5 g/t gold, 24 g/t silver, 5.5%
zinc and 0.3% copper. A 4 kilometre long geophysical line has
defined a 900 metre wide low resistivity anomaly below the
mineralized mantos. Two additional large lateral chargeability
anomalies exist to the west and east.
Sundae Prospect
Sundae is an epithermal system more than 3
kilometres long and 1 kilometre wide. Mechanized trenching has
discovered a silica cap with several associated sub-parallel vein
swarms that can be projected to depths of more than 350 metres in
the resistivity sections. The silica types and textures are typical
of the upper part of the epithermal system. Assays of up to 0.1 g/t
gold and 8 g/t silver were obtained from rock chip geochemical
sampling.
Mr. Randy Reifel, President states, “We are very
early in the drill program with only five holes completed in the
Central Prospect. We are very encouraged that Y-02 and Y-03 tested
a deep blind IP anomaly that underlies a 3.0 x 1.5 kilometre
hydrothermal system exposed on surface and confirms its continuity
to a depth of 500 metres. The strength and types of the alteration
with increasing copper values lower in the system indicates a
potential significant mineralized intrusive. We are also pleased
with the first two drill holes in the Spaniard zone. Drill results
confirmed the depth of the gold-silver sulfide mineralization to at
least 100 metres. Resistivity profiles indicate that several of
these structures may extend more than 350 metres below
surface.”
2018 Exploration
The Phase 1 drill program will be expanded to
test the Lucy, Yasmin and Sundae district scale prospects.
Petrographic, structural and mineralogic studies of the drill core
will characterize the hydrothermal systems and the mineralization
controls. A detailed 3D geophysical model is expected in January
for the 2017 IP/Resistivity surveys completed which will further
delineate untested sulfide and structural targets.
Presently, Chesapeake is well funded with $20
million in working capital.
ALS Global was the analytical laboratory used
for the samples included in this release. The split core sample
preparation was primarily performed in Guadalajara and Hermosillo,
Mexico and analysed in Vancouver, Canada. Certified standard and
blank samples were included every 25-30 samples for QA/QC purposes
depending on the length of the drill hole. The required analysis
were Fire Assay 30g with ICP finished for gold and ICP by 4 acid
digestion for 33 other elements.
Alberto Galicia, P. Geo, Vice President
Exploration for Chesapeake and a Qualified Person as defined by
NI43-101, has reviewed the technical information in this
release.
For more information on Chesapeake and its
Metates Project and regional exploration program, please visit our
website at www.chesapeakegold.com or contact investor relations at
604-731-1094.
CHESAPEAKE GOLD CORP
“P. Randy Reifel”
P. Randy ReifelPresident
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.
FORWARD LOOKING
STATEMENTS
This news release contains “forward-looking
information” within the meaning of applicable Canadian securities
legislation. Such forward looking statements and information herein
include, but are not limited to, statements regarding prospective
gold, silver and related metal production, timing and expenditures
to explore and develop prospective mineral properties, gold, silver
and related metal resources, grades and recoveries, cash costs per
ounce, capital and operating expenditures and sustaining capital
and the ability to fund mine development. The Company does not
intend to, and does not assume any obligation to update such
forward-looking statements or information, other than as required
by applicable law. Forward-looking statements or information
involve known and unknown risks, uncertainties and other factors
that may cause the actual results, level of activity, performance
or achievements of Chesapeake and its operations to be materially
different from those expressed or implied by such statements. Such
factors include, among others: ability to finance mine development,
fluctuations in the prices of gold, silver and zinc, fluctuations
in the currency markets (particularly the Mexican peso, Canadian
dollar and U.S. dollar); changes in national and local governments,
legislation, taxation, controls, regulations and political or
economic developments in Canada and Mexico; operating or technical
difficulties in mineral exploration, development and mining
activities; risks and hazards of mineral exploration, development
and mining(including environmental hazards, industrial accidents,
unusual or unexpected geological conditions, pressures, cave-ins
and flooding);inadequate insurance, or inability to obtain
insurance; availability of and costs associated with mining inputs
and labour; the speculative nature of mineral exploration and
development, diminishing quantities or grades of mineral reserves
as properties are mined; risks in obtaining necessary licenses and
permits, and challenges to the Company’s title to properties.
Although the Company has attempted to identify important factors
that could cause actual results to differ materially from those
contained in forward-looking statements or information, there may
be other factors that cause results to be materially different from
those anticipated, described, estimated, assessed or intended.
There can be no assurance that any forward- looking statements or
information will prove to be accurate as actual results and future
events could differ materially from those anticipated in such
statements or information. Accordingly, readers should not place
undue reliance on forward-looking statements or information.
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