Chesapeake Provides Update on Yarely and Tatatila Exploration
  finance.yahoo.com
    GlobeNewswire•December 13, 2018
  VANCOUVER,   British Columbia, Dec. 13, 2018 (GLOBE NEWSWIRE) -- Chesapeake Gold   Corp. (“Chesapeake” or “Company”) wishes to provide an update on the   exploration work at its 100% owned Yarely Project (“Yarely”) in Sinaloa   State and Tatatila Project (“Tatatila”) in Veracruz State, Mexico.   Yarely is located 25 kilometres west of the proposed Metates plant site   and encompasses 76,200 hectares. Metates is Chesapeake’s flagship   project which hosts one of the largest undeveloped gold, silver and zinc   reserves in the world. Tatatila is a district scale project hosting   gold-copper skarn mineralization which strategically surrounds Mexican   Gold Corp.’s Las Minas project.
  Yarely Project, Sinaloa
  In   early 2018, a Phase I drill program at Yarely tested three of six  known  prospects with the drill results and related exploration  activities  reported in June 2018. The drill program was successful in  the discovery  of a blind copper-molybdenum porphyry system at Loretos,  an extensive  near-surface polymetallic skarn at Lucy and a high grade  gold-silver  vein system at Spaniard-Central.
  During  the second  half of 2018, Chesapeake’s focus at Yarely was to explore  Los Mimbres  and advance the Sundae prospect to the drill stage. In  addition, the  Company conducted geological reconnaissance in the largely  unexplored  northeast and southwest areas of Yarely which led to the  discovery of  the Goyo epithermal prospect.
  Los Mimbres Prospect
  Widespread   rock chip channel sampling and preliminary geological mapping at Los   Mimbres defined a northeast trending vein swarm at least two kilometers   long and one kilometer wide, situated within a large regional corridor.   Sulfide bearing quartz veins and associated stockwork are mainly  hosted  within mudstones and intrusive rocks with silver-gold  mineralization and  occasional base metals. Topographically, the system  can be traced for  over 200 meters in elevation in an area of moderate  relief.   The vein  swarm remains open particularly to the southwest  where  higher grades  were more evident in the upper levels of the  system.
  Channel sampling of the different veins and stockwork returned the following results:
  7 meters of 1.15 g/t gold and 88 g/t silver 7 meters of 0.90 g/t gold and 87 g/t silver 5 meters of 0.11 g/t gold and 196 g/t silver 1 meter of 0.38 g/t gold, 98 g/t silver, 2.42% lead and 1.1% zinc 31 meters of 0.30 g/t gold and 14 g/t silver (stockwork around veins) 10 meters of 0.24 g/t gold and 5 g/t silver (stockwork around veins)
  Sundae Prospect
  Sundae   represents a well-preserved epithermal vein system over three   kilometers in length which hosts individual quartz veins from 1 to 5   metres wide.  These veins are commonly part of a vein swarm up to tens   of meters in width. The northwest-trending en-echelon veins are hosted   in Tertiary-age red beds and volcanic rocks.    
  The  chalcedonic  and sugary, fine-grained texture of the quartz veins  display classic  high level, low sulfidation epithermal textures  (multiple periods of  brecciation, banded texture, quartz after  calcite).  Petrographic and  fluid inclusion studies performed on surface  samples confirm the vein  mineralization formed at low temperatures,  below 180 degrees  centigrade, and at or near the current topographic  surface. Vein  samples from surface exposures up to 0.1 g/t gold and 8  g/t silver  suggest there are precious metals in the system. Epithermal  vein  deposits often show strong vertical zonation with low grade  precious  metals overlying Bonanza grade gold-silver zones at depths of  less than  a few hundred meters. 
  Goyo Prospect
  The  regional  reconnaissance and stream sediment geochemical program at  Yarely  located several additional areas with anomalous precious metals.   Amongst the target areas under further investigation is Goyo, a new   significant gold-silver prospect discovered in southwest Yarely.
  The   Goyo prospect is situated along the west flank of a set of regional   size ring structures hosting other gold-silver targets within volcanic   rocks to the northeast and southeast, all part of an extensive district   scale epithermal system associated with a possible dome field.    Mineralization at Goyo comprises low sulfidation epithermal quartz   breccias and stockworks related to north-south trending regional   structures over one kilometer long associated with the contact of a   Tertiary-age rhyolite flow dome and andesites.
  Assays from two rock chip channel sections taken 100 meters apart returned:
  30 meters of 1.63 g/t gold and 38 g/t silver  15 meters of 0.60 g/t gold and 9 g/t silver
  Another   subparallel gold-silver mineralized structure located two kilometers  to  the northwest returned the following chip channel assays across  quartz  veins:
  4 meters of 3.74 g/t gold and 90 g/t silver 5 meters of 1.30 g/t gold and 15 g/t silver  25 meters of 0.54 g/t gold and 35 g/t silver in stockworks adjacent to veins
  Further   to the south from Goyo, field work has recently identified an argillic   alteration zone 1,000 by 500 meters hosting quartz stockwork.  Chesapeake  recently expanded its land position by staking 4,200  hectares covering  this new prospective area.    
  Tatatila Project, Veracruz
  In   2007, Chesapeake acquired Tatatila through the purchase and staking of   15,000 hectares in Veracruz State. During 2007-2008, Chesapeake’s   reconnaissance program identified several gold-copper skarn prospects   that are similar to the Torex Gold deposits in the Guerrero Gold Belt.    The Tatatila concessions surround Mexican Gold Corp’s Las Minas Project   with a reported NI43-101 resource of 1 million ounces at a grade of 2   g/t gold equivalent in two separate zones.
  The  skarns at  Tatatila are similar to those at Las Minas, consisting of  tabular and  podiform, garnet-magnetite-pyroxene bodies mineralized with   chalcopyrite-pyrite-bornite and developed along the contact between   dioritic intrusives and limestones.  The skarns bodies are locally zoned   ranging from gold-copper rich proximal to the contact with mostly   copper-zinc in the more distal areas.
  In the third quarter,   Chesapeake commenced a follow-up exploration program at Tatatila to   determine the potential extension of the Las Minas skarn zones along   regional limestone-intrusive contacts and associated structural trends.   Geological interpretation, rock chip channel sampling and a magnetics   geophysical survey extended known and discovered new gold-copper-zinc   mineralized skarn bodies along a 3 kilometer southeast trending corridor   from Las Minas. So far, four zones, namely La Paulina, La Esperanza,   Tenepanoya and Galdy have been defined. Rock chip channel sampling   results include the following from 2018 and 2007 (where indicated):
  La Paulina  
  12 meters of 3.0 g/t gold, 12 g/t silver and 0.24% copper 6 meters of 5.1 g/t gold, 12 g/t silver and 0.46% copper 18 meters of 3.8 g/t gold, 7 g/t silver and 0.50% copper (sampled 2007) 11 meters of 0.24 g/t gold, 37 g/t silver and 12.95% zinc (sampled 2007)
  La Esperanza 
  12 meters of 1.0 g/t gold, 0.35% copper and 0.22% zinc  6 meters of 0.30 g/t gold, 0.12% copper and 2.05% zinc  12 meters of 0.50 g/t gold, 0.40% copper, 0.70% zinc (sampled 2007)
  Tenepanoya
  9 meters of 2.3 g/t gold, 8 g/t silver and 0.30% copper  11 meters of 1.4 g/t gold, 0.47% copper 12 meters of 0.20 g/t gold, 0.11% copper and 1.13% zinc
  Galdy 
  9 meters of 0.90 g/t gold, 14 g/t silver and 2.0% copper (sampled 2007)
  Generative   regional exploration was also undertaken elsewhere along the favorable   limestone-intrusive contact where prospective skarn deposits are known   to occur.  Exploration along irregular and extensive contact zones led   to the skarn discoveries at Melany in 2007 and Plan de Gallo  this   year.  Melany and Plan de Gallo form a northwest-trending   intrusive-limestone corridor five kilometers long and remains open.    Plan de Gallo comprises at least three gold-copper mineralized skarn   zones which are 500 meters apart.  Rock chip channel sampling sections   returned the following results: 
  Melany
  67 meters of 1.6 g/t gold, 7 g/t silver and 0.60% copper
  Plan de Gallo 
  21 meters of 2.2 g/t gold, 5 g/t silver and 0.27% copper  15 meters of 2.3 g/t gold, 6 g/t silver and 0.30% copper  9 meters of 1.2 g/t gold, 6 g/t silver and 0.25% copper  11 meters of 1.4 g/t gold, 7 g/t silver and 0.36% copper  8 meters of 1.0 g/t gold, 10 g/t silver and 1.25% copper
  Additionally,   precious and base metal stream sediment anomalies have been defined   north and east of the Melany-Plan de Gallo trend over an area exceeding   1,500 hectares. This region has favorable limestone-intrusive contacts   and underscores the very prospective potential of Tatatila.
  Tatatila   remains largely unexplored and the lithological and structural   characteristics are extremely favorable for discovering additional skarn   zones along with associated polymetallic replacement, intrusive hosted   and vein type mineralization.  Recognizing the Las Minas discovery,   Tatatila is an emerging district hosting several mineralized zones that   could develop into a multi-million ounce gold equivalent camp close to   established infrastructure.
  2019 Exploration 
  At   Yarely, the Goyo prospect will be systematically advanced to the drill   stage as well as follow-up exploration in several areas showing   anomalous stream sediments.  Yarely continues to be an emerging,   diversified mineralized camp with multiple district scale prospects and   the potential for future discoveries.
  Eleven  kilometers  southeast of Metates, a detailed program of geological  mapping,  sampling and an IP. Resistivity survey is planned for the San  Javier  Project. San Javier is a large gold-silver disseminated and  stockwork  system hosted in sandstone and intrusive rocks which at depth,  might  transition into sulfide mineralization similar to Metates.
  Chesapeake is well funded with $17.5 million in cash and marketable securities.
  ALS   Global and SGS were the analytical laboratories used for the samples   included in this release. The samples sent to ALS were crushed and   ground and a representative sample split was sent to Vancouver, Canada   for assaying using ALS methods Au-ICP21 and ME-ICP61. Samples sent to   SGS were prepared and analyzed at its facilities in Durango, Mexico   using Au-FAA and ICP methods.     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, the 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 Reifel President
  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. |