{"id":207447,"date":"2017-07-24T08:10:28","date_gmt":"2017-07-24T12:10:28","guid":{"rendered":"http:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/mandalay-resources-provides-exploration-results-for-the-first-half-of-2017-globenewswire-press-release\/"},"modified":"2017-07-24T08:10:28","modified_gmt":"2017-07-24T12:10:28","slug":"mandalay-resources-provides-exploration-results-for-the-first-half-of-2017-globenewswire-press-release","status":"publish","type":"post","link":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/life-extension\/mandalay-resources-provides-exploration-results-for-the-first-half-of-2017-globenewswire-press-release\/","title":{"rendered":"Mandalay Resources Provides Exploration Results for the First Half of 2017 &#8211; GlobeNewswire (press release)"},"content":{"rendered":"<p><p>July 24, 2017 07:30 ET |    Source: Mandalay Resources Corporation      <\/p>\n<p>    TORONTO, July 24, 2017 (GLOBE    NEWSWIRE) -- Mandalay Resources Corporation (\"Mandalay\" or the    \"Company\") (TSX:MND) is pleased    to provide exploration updates for the first half of 2017 for    two of its producing properties, Bjrkdal (Sweden) and    Costerfield (Australia), and its Challacollo (Chile)    development project. <\/p>\n<p>    This press release refers to    tables and figures. Accompanying tables can be found at the end    of this press release, whereas the figures accompanying this    release can be found in an exploration presentation posted on    the Companys website that can be accessed at:  <\/p>\n<p>    <a href=\"http:\/\/www.mandalayresources.com\/investor-presentations\/#Technical_Presentations\" rel=\"nofollow\">http:\/\/www.mandalayresources.com\/investor-presentations\/#Technical_Presentations<\/a>  <\/p>\n<p>    Dr. Mark Sander, President and CEO    of Mandalay, commented, In the first half of 2017, our    exploration programs yielded excellent results, which clearly    demonstrate the potential for significant near-term and    long-term Mineral Reserve additions at both Bjrkdal and    Costerfield.  <\/p>\n<p>    At Bjrkdal, extensional drilling    to the northeast and north of the mine demonstrated that the    gold mineralized system extends several hundred metres beyond    the current mine in those directions and is not yet closed    off. As a result, we have demonstrated the potential to    increase Mineral Reserves at Lake Zone underground and West Pit    at surface. We have also made significant progress in    understanding the distribution and characteristics of    high-grade skarn mineralization that occurs both in the open    pit and underground mines. Follow-up drilling is    planned.  <\/p>\n<p>    At Costerfield, drilling has    improved the outlook for mine life extensions at different    scales. At Brunswick, new holes have delivered high-grade, deep    intersections that are expected to make a positive impact on    the updated Mineral Resource and Reserve model anticipated in    the fourth quarter. As previously reported, we anticipate the    new model will significantly extend mine life based on our    expectation that Brunswick will prove to be economic. As well,    the potential next major new mineralized shoot after Brunswick    has begun to emerge in our new drilling below the historic    workings on the main Costerfield lode. These intercepts contain    extraordinary gold and antimony grades scattered along a 400    metre strike length and 100 metre vertical interval. New    intercepts along N-lode have also identified new splays which,    as we follow them up, have the potential for incrementally    adding Reserves near current underground    infrastructure.  <\/p>\n<p>    Dr. Sander concluded, Lastly, at    Challacollo, we reached a major milestone with the discovery of    sufficient water to support an eventual operation.    Activities to permit and complete a production well, followed    by transfer of existing water rights to the new location are    underway. We now have the option to launch a project to    optimize previously estimated capital and operating costs for a    mine and plant at Challacollo.  <\/p>\n<p>    Bjrkdal    Exploration  <\/p>\n<p>    Significant Exploration Results (Tables 1 through 4; Figures 1    through 5)  <\/p>\n<p>    Underground Exploration  <\/p>\n<p>    In the first half of 2017, underground diamond drilling at    Bjrkdal extended the north-eastern limit of the Bjrkdal    vein-system and infilled discrete areas. Intercepts from the    extensional drilling demonstrate that gold mineralization    extends along-strike from the defined resource for at least    200-300 metres (Figure 2 and Table 2) and mineralization    remains open to the north and east. Infill drilling also    increased confidence and delivered some high-grade intercepts    in areas closer to the current limits of the mine (Figure 3 and    Table 3).  <\/p>\n<p>    Open Pit Exploration  <\/p>\n<p>    Near-mine surface drilling with both core and Reverse    Circulation methods during the first half of 2017 focused on    extending gold mineralization in the north-western portions of    the West Pit (Figure 4). This drilling intercepted many new    mineralized intervals in the northern wall of the West Pit    (Table 4). Results from this extensional drilling demonstrate    that the mineralized vein-system in this area of the deposit    extends from the current limits of the West Pit to at least 150    m further to the north. These veins are interpreted to    correlate with the same vein-system mined from the underground    mine, located to the east of this area. Therefore, the    Bjrkdal vein-system remains open to the west and north-west of    the current mine footprint, presenting high-calibre extensional    targets for future exploration programs at Bjrkdal.  <\/p>\n<p>    In addition to successful extensional drilling of the Bjrkdal    vein-system, significant gold intercepts were also obtained    from non-veined, mineralized carbonate lenses belonging to the    host-stratigraphy (the Bjrkdal marble unit). These mineralized    carbonate lenses are strongly altered, containing abundant    amphiboles (predominately actinolite), silica and chlorite with    accessory pyrite, pyrrhotite and pyroxenes. This metasomatic    assemblage suggests skarn-like depositional mechanisms, and    represents an exciting new deposit-type both within and    peripheral to the footprint of the current Bjrkdal mine.  <\/p>\n<p>    Three gold-bearing, skarn-like bodies have been defined though    drilling over the past six months; two in the vicinity of the    underground mine and a single in the open pit mine (Figure 5).    The skarnified carbonate lenses are shallow dipping, narrow,    plunging bodies that are located above and adjacent to the    Bjrkdal vein-system. Intercepts of this skarn-hosted    gold-mineralization include:  <\/p>\n<p>    These results suggest that this style of mineralization    presents the possibility of bulk-minable tonnages of    potentially much higher gold-concentrations than the more    typical Bjrkdal vein systems. Within the month of June, a    1,176 tonne parcel of the recently exposed West Pit skarn ore    was crushed and milled with results indicating a    back-calculated head-grade of 4.30 g\/t Au. The recent    intercepts of all significant gold-bearing skarn intercepts    will be followed up as priority targets in the remainder of    2017 and 2018 exploration programs, while regional exploration    models and programs will be refined to incorporate further    targeting of near-surface, high-grade gold skarn and skarn-like    mineralized systems in the larger Bjrkdal area.  <\/p>\n<p>    Bjrkdal Drilling, Sampling and    Assaying  <\/p>\n<p>    During the period from January 1, 2017 to June 30, 2017, a    total of 13,640 metres of exploration drilling was completed in    66 drill holes. Drilling included 23 surface core and RC    holes totalling 3,451 m and 43 underground core holes totalling    10,189 m. All drill-hole collars are surveyed, and downhole    surveys are completed in order to record hole azimuth and dip    variations.  <\/p>\n<p>    All surface and underground exploration drilling has been    conducted by third party contractors, with a mix of core and    reverse circulation drilling using WL66, NQ2, HQ and 5 RC    sized drilling equipment (producing 50 mm, 50.5 mm and 63.5 mm    diameter core respectively).  <\/p>\n<p>    Core and RC samples are logged by Mandalay geologists on-site.    Assaying of Bjrkdal samples was completed at CRS Minlab Oy    (CRS) in Kempele, Finland and ALS in Pite, Sweden. Whole core    samples (WL66 and NQ2 size) were sent directly to the    independent laboratories for sample preparation and assaying,    while HQ diameter core was half-sawn at the laboratories    off-site before sample preparation. Assaying was conducted    utilizing the Pal1000 (CRS) and LeachWELL (ALS) cyanide    leaching processes. Mandalays rigorous QA\/QC program includes    the use of standard reference samples, blanks, duplicates,    repeats, and internal laboratory quality assurance procedures.    More details on the drilling, logging, sampling, and assaying    procedures are contained in the Technical Report Mandalay    Resources Corporation Technical Report on the Bjrkdal Gold    Mine, Sweden filed on SEDAR (www.sedar.com) on January 27, 2017.  <\/p>\n<p>    Costerfield    Exploration  <\/p>\n<p>    Significant Exploration Results (Tables 5 through 8; Figures 6    through 12)  <\/p>\n<p>    Brunswick        Following structural analysis of Brunswick mineralization, the    Company conducted infill drilling within the Penguin to Kiwi    (PK) panel of the Brunswick lode (Table 6 and Figure 7).    Further confidence of grade continuity was gained through this    drilling, with high-grade intercepts including 24.4 g\/t Au and    6.1% Sb over a vein width of 2.01 m in BD278W2.  <\/p>\n<p>    These results will be reflected in a resource update expected    in the fourth quarter of 2017. This drilling is expected to    result in an increase in Indicated Mineral Resource of the    Brunswick lode.  <\/p>\n<p>    Further drilling was undertaken with the purpose of extending    Brunswick below the Kiwi Fault and to the south. Both drilling    campaigns intercepted antimony and gold mineralization along    the Brunswick corridor. Mineralization has now been identified    approximately 280 m below historic workings and approximately    100 m below the current Inferred Mineral Resource. Below the    historic B3 pit, the Brunswick line of mineralization has been    identified at a depth of 225 m below surface and over a strike    length of 300 m (Figure 7). Highlights of this extension    drilling are:  <\/p>\n<p>    Future exploration efforts are expected to focus on extending    the current Mineral Resource below the Kiwi fault and into    Brunswick South, pending economic analysis.  <\/p>\n<p>    Costerfield  <\/p>\n<p>    A target testing campaign investigating the continuation of    mineralization underneath the historic Costerfield mine    workings is currently underway. The early stages of this    campaign have shown great success with mineralization confirmed    over a strike length of approximately 500 m and to a depth of    approximately 150 m vertically below the current workings    (Figure 8). The highlight of the program during the first half    of 2017 is the deepest northern intercept, which contained 59.8    g\/t Au and 3.2% Sb over a true vein width of 0.56 m in BC006w1    (Table 7).  <\/p>\n<p>    N Lode Upper  <\/p>\n<p>    Structural analysis of the mineralized corridor known as N Lode    has led to the recognition of a previously untested prospective    zone near to surface. The first drill hole to test this area    has confirmed the presence of an up-dip continuity to the    enriched northern portion of N Lode. The proximity of this    mineralization to established underground development makes    this find an important focus for near future delineation    drilling (Table 8 and Figure 9).  <\/p>\n<p>    Alison South  <\/p>\n<p>    Testing of the upper portion of mineralization over the Cuffley    Deposit has returned high-grade gold results within two veins    in an offset, up-dip continuation of the Cuffley Deposit named    Alison South. The highlight of this drilling was an intercept    containing 71.1 g\/t Au and 0.5% Sb over a true vein width of    0.35 m in AD168 (Table 8 and Figure 10).  <\/p>\n<p>    K Lode  <\/p>\n<p>    A high-grade portion of K Lode was discovered through the    opportunistic drilling program (Table 8 and Figure 11). This    vein has already been accessed through mining on an    intersecting portion of N Lode which makes this a potential    low-cost mining source in the near future.  <\/p>\n<p>    Augusta East  <\/p>\n<p>    A drilling campaign investigating the possibility of an eastern    repetition of the Augusta and Cuffley line of mineralization is    currently underway. Gold has been located within a    near-surface, sub-vertical vein set in the first hole to be    drilled on this target (Figure 12). Although the grade of these    intercepts are not potentially economic, they are    characteristic of the periphery of orebodies in the district.    Follow-up drilling is planned.  <\/p>\n<p>    Costerfield Drilling, Sampling, and Assaying  <\/p>\n<p>    During the first half of 2017, Mandalay drilled 18,489 m of    diamond core at its Costerfield gold-antimony mine (Table 5).    5,520 m was dedicated to increasing immediate mine life through    infill and extension of the Brunswick resource and through    opportunistic drilling projects on K Lode, N Lode and Alison    South. 12,969 m was devoted to regional exploration, with the    drill testing of the Costerfield Mine extension, Augusta East    and Brunswick line of lode extension. In addition, the Company    completed 1,652 m of on-vein operating development and    associated sampling of N Lode, Cuffley Lode, New Vein, Bob lode    and associated splays.  <\/p>\n<p>    Drill core was logged and sampled by Costerfield geologists,    who also mapped and sampled the development advances. All    samples were sent to Onsite Laboratory in Bendigo, Victoria,    Australia for sample preparation and assay. Site geological and    metallurgical personnel have implemented a QA\/QC process that    includes the regular submission of standard reference materials    and blanks with drill and face samples submitted for assay.    Standard reference materials have been certified by Geostats    Pty Ltd. (see Technical Report entitled Costerfield Operation,    Victoria, Australia NI 43-101 Report, filed on SEDAR (www.sedar.com) March 31, 2017, which    contains a complete description of drilling, sampling, and    assaying procedures).  <\/p>\n<p>    Challacollo    Exploration  <\/p>\n<p>    Four holes were drilled at Challocollo during the first half of    2017 to explore for water, a critical requirement for further    project development. A total of 416.5 metres was drilled, with    all four holes encountering promising quantities of water.    Drill hole locations are provided in Figure 13, with pump test    results in Table 9.  <\/p>\n<p>    Qualified Person:  <\/p>\n<p>    Chris Gregory, Vice President of Operational Geology and    Exploration at Mandalay Resources, is a Member of the    Australian Institute of Geoscientists (AIG), and a Qualified    Person as defined by NI 43-101. He has reviewed and approved    the technical and scientific information provided on all the    Companys properties contained in this release.  <\/p>\n<p>    About Mandalay Resources    Corporation:  <\/p>\n<p>    Mandalay Resources is a Canadian-based natural resource company    with producing assets in Australia, Sweden and producing and    exploration projects in Chile. The Company is focused on    executing a roll-up strategy, creating critical mass by    aggregating advanced or in-production gold, copper, silver and    antimony projects in Australia, the Americas and Europe to    generate near-term cash flow and shareholder value.  <\/p>\n<p>    Forward-Looking    Statements:  <\/p>\n<p>    This news release contains \"forward-looking statements\"    within the meaning of applicable securities laws, including    statements regarding expected exploration results and increases    to resources and reserves. Readers are cautioned not to place    undue reliance on forward-looking statements. Actual results    and developments may differ materially from those contemplated    by these statements depending on, among other things, changes    in commodity prices and general market and economic conditions.    The factors identified above are not intended to represent a    complete list of the factors that could affect Mandalay. A    description of additional risks that could result in actual    results and developments differing from those contemplated by    forward-looking statements in this news release can be found    under the heading Risk Factors in Mandalays annual    information form dated March 31, 2017, a copy of which is    available under Mandalays profile at <a href=\"http:\/\/www.sedar.com\" rel=\"nofollow\">http:\/\/www.sedar.com<\/a>. In    addition, there can be no assurance that any inferred resources    that are discovered as a result of additional drilling will    ever be upgraded to proven or probable reserves. Although    Mandalay has attempted to identify important factors that could    cause actual actions, events or results to differ materially    from those described in forward-looking statements, there may    be other factors that cause actions, events or results not to    be as anticipated, estimated or intended. There can be no    assurance that forward-looking statements will prove to be    accurate, as actual results and future events could differ    materially from those anticipated in such statements.    Accordingly, readers should not place undue reliance on    forward-looking statements.  <\/p>\n<p>    Accompanying Drill Summary    Tables:  <\/p>\n<p>    Table 1: Bjrkdal H1 2017 drilling summary  <\/p>\n<p>    Table 2: Bjrkdal underground extensional drilling    results  <\/p>\n<p>    Significant new underground core-drilling intercepts from    extensional drilling. Note: only intercepts displayed with Au    grade greater than resource cut-off grade (i.e. greater than    underground resource cut-off grade once diluted to minimum    mining width of 3 metres). Drill holes labelled with italics    and * are skarn-hosted intercepts.  <\/p>\n<p>          Hole ID        <\/p>\n<p>    Table 3: Bjrkdal underground infill    drilling results  <\/p>\n<p>    Significant new underground core-drilling intercepts from    infill drilling. Note: Only intercepts included with Au grade    that is greater than resource cut-off grade (i.e. greater than    underground resource cut-off grade once diluted to minimum    mining width of 3 metres).  <\/p>\n<p>          Hole ID        <\/p>\n<p>    Table 4: Bjrkdal significant new open pit core-drilling    (MP-7 series) and reverse circulation (MR-7 series) intercepts    from extensional drilling  <\/p>\n<p>    Note: only Au grade is displayed that is greater than resource    cut-off grade (i.e. greater than underground resource cut-off    grade once diluted to minimum mining width of 2 metres). Drill    holes labelled with italics and * are skarn intercepts.  <\/p>\n<p>          Hole ID        <\/p>\n<p>    Table 5: Costerfield H1 2017 drilling summary  <\/p>\n<p>    Table 6: Brunswick lode significant intercepts  <\/p>\n<p>    Note:    - Raw, undiluted assay intervals are reported that occur within    diluted intervals that contain greater than 1 AuEq g\/t over a    minimum mining width of 1.8 m.    - True width is preliminary estimate only and may not reflect    final true width used in resource estimation    - AuEq (g\/t) = Au (g) + Sb (%) x(Price per 10 Sb(kg)  Sb    Recovery(%))\/(Price per 1 Au(g)  Au Recovery (%))  <\/p>\n<p>    Table 7: Costerfield lode significant    intercepts  <\/p>\n<p>    Note:    - True width is preliminary estimate only and may not reflect    final true width used in resource estimation    - AuEq (g\/t) = Au (g) + Sb (%) x(Price per 10 Sb(kg)  Sb    Recovery(%))\/(Price per 1 Au(g)  Au Recovery (%))<\/p>\n<p>    Table 8: Opportunistic drilling significant    intercepts  <\/p>\n<p>    Note:    - Raw, undiluted assay intervals are reported that occur within    diluted intervals that contain greater than 1 AuEq g\/t over a    minimum mining width of 1.8 m.    - True width is preliminary estimate only and may not reflect    final true width used in resource estimation    - AuEq (g\/t) = Au (g) + Sb (%) x(Price per 10 Sb(kg)  Sb    Recovery(%))\/(Price per 1 Au(g)  Au Recovery (%))<\/p>\n<p>    Table 9: Challacollo pump test results  <\/p>\n<\/p>\n<p>      Related Articles    <\/p>\n<p><!-- Auto Generated --><\/p>\n<p>Read more: <\/p>\n<p><a target=\"_blank\" rel=\"nofollow\" href=\"https:\/\/globenewswire.com\/news-release\/2017\/07\/24\/1056064\/0\/en\/Mandalay-Resources-Provides-Exploration-Results-for-the-First-Half-of-2017.html\" title=\"Mandalay Resources Provides Exploration Results for the First Half of 2017 - GlobeNewswire (press release)\">Mandalay Resources Provides Exploration Results for the First Half of 2017 - GlobeNewswire (press release)<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p> July 24, 2017 07:30 ET | Source: Mandalay Resources Corporation TORONTO, July 24, 2017 (GLOBE NEWSWIRE) -- Mandalay Resources Corporation (\"Mandalay\" or the \"Company\") (TSX:MND) is pleased to provide exploration updates for the first half of 2017 for two of its producing properties, Bjrkdal (Sweden) and Costerfield (Australia), and its Challacollo (Chile) development project. This press release refers to tables and figures.  <a href=\"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/life-extension\/mandalay-resources-provides-exploration-results-for-the-first-half-of-2017-globenewswire-press-release\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":5,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[187736],"tags":[],"class_list":["post-207447","post","type-post","status-publish","format-standard","hentry","category-life-extension"],"_links":{"self":[{"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/posts\/207447"}],"collection":[{"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/users\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/comments?post=207447"}],"version-history":[{"count":0,"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/posts\/207447\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/media?parent=207447"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/categories?post=207447"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/tags?post=207447"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}