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Dunav Resources Announces the Discovery of a New Gold-Silver-Base Metal Epithermal System, Part of the Tulare Project

Jan 9 2013 12:00AM

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LONGUEUIL, QUEBEC -- (Marketwire) -- 01/09/13 -- Dunav Resources Ltd. (TSX VENTURE: DNV) (the "Company" or "Dunav") is pleased to present an exploration update on its 100% held Tulare Copper-Gold Porphyry Project located in Southern Serbia.

1.  HIGHLIGHTS--  Late in the 2012 field season, four very wide-spaced diamond drill holes    were completed on the Bakrenjaca carbonate-base metal gold epithermal    system which is located 3 km south from the Kiseljak copper-gold    porphyry deposit. All four drill holes intersected epithermal-style    mineralization.--  Results have now been returned from this initial 'scout' drilling    program which was designed to follow-up on encouraging surface trench    results. The area of mapped alteration and epithermal mineralization    covers an area of approximately 1.5 km x 1 km and significant    intersections are listed below, calculated using a 0.4 g/t AuEq cut-off    grade:----------------------------------------------------------------------------              From     To Interval     Au     Ag     Cu     Pb     Zn   AuEqHole ID        (m)    (m)      (m)  (g/t)  (g/t)    (%)    (%)    (%)  (g/t)----------------------------------------------------------------------------BKDD001         36     40        4   0.48   5.53   0.03   0.46   0.38   0.96BKDD001         64     68        4   0.11   5.85   0.11   0.07   0.05   0.43BKDD001        100    111       11   5.13    346   1.19   2.36   1.86   14.5BKDD001        116    127       11   0.37   7.82   0.08   0.23   0.88   1.09BKDD002          9     16        7   0.48   1.34   0.00   0.07   0.86   0.89BKDD002         28     31        3   0.50   0.88   0.00   0.05   0.12   0.59BKDD002         35     42        7   0.84   1.10   0.01   0.04   0.10   0.93BKDD002         49     79       30   0.36   1.70   0.01   0.12   0.28   0.58BKDD002        132    137        5   0.07   1.10   0.03   0.18   0.83   0.55GUDD001         80     85        5   0.14   4.14   0.04   0.24   0.34   0.52GUDD001         95     98        3   0.19   5.97   0.01   0.56   0.14   0.60GUDD001        156    160        4   0.23   6.70   0.01   0.20   0.12   0.49GUDD001        170    173        3   0.11   3.77   0.05   0.18   0.32   0.45GUDD001        178    182        4   0.15   7.58   0.05   0.57   0.47   0.78GUDD001        231    235        4   0.49   6.82   1.12   0.05   0.01   2.41GUDD001        296    317       21   0.11   4.91   0.07   0.85   1.13   1.12GUDD001        323    326        3   0.01   2.87   0.07   0.78   2.40   1.48GUDD001        447    452        5   0.03   0.76   0.05   0.27   0.46   0.42GUDD002         11     15        4   0.20   2.10   0.00   0.22   0.33   0.46GUDD002         35     39        4   1.03   13.3   0.05   0.84   1.45   2.28GUDD002         47     51        4   0.10   8.77   0.06   0.27   0.22   0.55GUDD002        141    144        3   0.10   1.79   0.00   0.34   1.60   0.93---------------------------------------------------------------------------- - 0.4 g/t AuEq cut-off ($1,500/oz. Au, $25/oz Ag, $3.50/lb. Cu,   $0.90/lb. Pb, $0.90/lb. Zn), 3 m minimum composite length, 3 m maximum   internal dilution.   -- AuEq = ((Au g/t x 48.226)+(Ag g/t x 0.8038)+(Cu% x 77.16)+(Pb% x   19.84)+(Zn% x 19.84)) / 48.226 - Diamond drill samples are PQ, HQ or NQ half core, using a nominal 1m   sampling basis and weigh approx. 3-6 kg. - Assay method: Fire assay Au (50 g); Ag, Cu, Pb & Zn by aqua regia   digestion with AAS and/or ICPMS finish. - Intercept widths do not necessarily represent true width. - No top cut applied.--  The recently announced Kiseljak copper-gold mineral resource, prepared    by AMC Consultants Limited (UK), an independent mining consulting firm,    has been estimated at 300,500,000 tonnes grading an average of 0.27%    copper and 0.26 g/t gold in the inferred resource category for 1.8    billion pounds of copper and 2.5 million ounces of gold, using a 0.25%    copper equivalent cut-off.--  The Tulare Copper-Gold Porphyry Project comprises several porphyry    copper-gold targets including Kiseljak, Yellow Creek, Trlica and    Calovica vis South and also includes the Bakrenjaca carbonate-base metal    gold epithermal vein system; all target areas are located within 3,000    meters of the Kiseljak deposit (refer to Figure 1). Dunav controls 100%    of this newly identified porphyry cluster, located within the Lece    Volcanic Complex.--  G Mining Services Inc. (Montreal) have been contracted to manage the    Preliminary Economic Assessment (PEA) of the Tulare Copper-Gold Porphyry    Project.2.  TRENCHING AT BAKRENJACA--  First pass exploration trenching was completed at Bakrenjaca based on    the detailed soil geochemistry (nominal 100 meter by 25 meter grid)    which had previously outlined a strongly anomalous Au-Ag-Cu-Pb-Zn zone    over an approximate area of 1.5 km by 1 km. Individual soil samples    returned up to 5.37 g/t Au, 39.3 g/t Ag, 0.58% Cu, 1.35% Pb and 0.62% Zn    (refer to Figure 4).--  It should be noted that the initial first pass trenching program was    largely predicated on areas where access was readily available; all    significant intersections are listed below, calculated using a 0.4 g/t    AuEq cut-off grade:----------------------------------------------------------------------------              From     To Interval     Au     Ag     Cu     Pb     Zn   AuEqTrench ID      (m)    (m)      (m)  (g/t)  (g/t)    (%)    (%)    (%)  (g/t)----------------------------------------------------------------------------BKTR003          0      3        3   0.38   6.50   0.01   0.41   0.20   0.75BKTR003         16     19        3   0.12   3.80   0.01   0.30   0.30   0.44BKTR005          4      8        4   0.04   0.63   0.00   0.15   1.02   0.54BKTR006          6     15        9   0.20   1.13   0.00   0.17   0.26   0.40BKTR007          6     19       13   0.23   1.11   0.01   0.33   0.76   0.71BKTR011         30     46       16   0.53   1.06   0.00   0.24   0.11   0.69BKTR012         14     23        9   0.32   0.96   0.02   0.17   0.79   0.76BKTR013          1      6        5   0.89   10.1   0.11   0.54   0.11   1.50BKTR014          0      8        8   0.04   0.75   0.97   0.09   0.13   1.69BKTR015          1     23       22   0.39   8.02   0.08   0.40   0.68   1.10BKTR016         56     71       15   0.44   2.85   0.01   0.19   0.05   0.61BKTR018         20     36       16   0.16   14.3   0.29   0.36   0.17   1.08BKTR019          0     46       46   0.48   16.4   0.21   0.28   0.69   1.50BKTR021          0     15       15   0.25   5.03   0.11   0.67   0.04   0.80BKTR021         21     27        6   0.11   1.67   0.04   0.52   0.03   0.42BKTR021         34     41        7   0.57   4.29   0.06   0.81   0.06   1.09BKTR021         50     55        5   0.55   8.50   0.06   0.70   0.01   1.07BKTR021         80     84        4   0.18   4.08   0.05   0.29   0.01   0.45BKTR022          3     26       23   1.03   11.6   0.31   2.65   0.37   2.96BKTR023          4     15       11   0.18   2.72   0.08   0.47   0.09   0.58-----------------------------------------------------------------------------  0.4 g/t AuEq cut-off ($1,500/oz. Au, $25/oz Ag, $3.50/lb. Cu, $0.90/lb.   Pb, $0.90/lb. Zn), 3 m minimum composite length, 3m maximum internal   dilution.   -- AuEq = ((Au g/t x 48.226)+(Ag g/t x 0.8038)+(Cu% x 77.16)+(Pb% x   19.84)+(Zn% x 19.84)) / 48.226-  Trench samples are designed to replicate HQ half core, using a nominal 1m   sampling basis and weigh approx. 3-6 kg.-  Assay method: Fire assay Au (50 g); Ag, Cu, Pb & Zn by aqua regia   digestion with AAS and/or ICPMS finish.-  Intercept widths do not necessarily represent true width.-  No top cut applied.--  Dunav has since extended the exploration trenching program to cover    larger areas of interest that have become apparent following the 2012    drilling and mapping program. These trench sampling results are expected    to be available during Q1 2013.--  Refer to Table 2 for a summary of all exploration trench intersections    at various AuEq cut-off grades for all Bakrenjaca trenches to date;    BKTR001 to BKTR024.--  Refer to Figure 2 for the location of all trenching and diamond drilling    completed to date within the Bakrenjaca mineralized 'footprint' and to    Figure 3 for a representative cross-section through the Bakrenjaca    target area.3.  DRILLING AT BAKRENJACA--  Four diamond drill holes have been completed at Bakrenjaca for a total    of 1,051.6 meters.--  All four drill holes intersected epithermal-style mineralization, which,    given the initial wide-spaced 'scout' drill hole spacing, may be viewed    as very encouraging.--  In general, the level of surface oxidation is low with sulfide    mineralization commencing within 10 meters of the surface.--  Drill hole GUDD001 (498.7 m) was the deepest hole drilled into the    target area and it is of particular interest that epithermal-style    mineralization was intersected throughout the drill hole, which    indicates that there is epithermal mineralization occurring over a    minimum 400 meters vertical extent within the Bakrenjaca target area.--  Refer to Figure 2 for the location of all trenching and diamond drilling    completed to date within the Bakrenjaca mineralized 'footprint' and to    Figure 3 for a representative cross-section through the Bakrenjaca    target area.--  Refer to Table 1 for a summary of all exploration diamond drill hole    intersections at various AuEq cut-off grades for all Bakrenjaca drill    holes to date (BKDD001 to BKDD002 and GUDD001 to GUDD002).4.  GEOLOGY AND MINERALIZATION STYLE--  The Bakrenjaca carbonate-base metal gold epithermal vein system is    located approximately 3 km south of the Kiseljak deposit and comprises    east-west trending corridors of sheeted to stockwork manganese carbonate    +/- quartz gold-silver-base metal veins hosted within argillic    (sericite-illite-smectite) altered andesitic volcanics, volcaniclastics    and sediments. Mapped zones of mineralization at surface range from less    than one meter to greater than thirty meters width.--  Based on this initial drilling program Dunav has noted two differing    styles of epithermal mineralization:    --  'Hangingwall-style' mineralization associated with manganese        carbonate (rhodochrosite) +/- quartz/chalcedony veining within the        volcano-sedimentary package which contains Au-Ag-Pb-Zn (sphalerite,        galena and pyrite) mineralization and display typical epithermal        textures such as colloform-crustiform banding.    --  'Footwall-style' mineralization as evidenced by BKDD001 (100-111m)        which has high grade Au-Ag-Cu-Pb-Zn mineralization and is located at        the low angle contact between the metamorphic basement (gneiss) and        the overlying volcano-sedimentary package. Carbonate replacement        textures (bladed quartz) indicative of boiling are evident within        this high grade zone.--  See Figure 3 for a representative cross-section through the Bakrenjaca    target area.5.  DISCUSSION--  Carbonate-base metal-gold epithermal deposits represent some of the most    prolific gold producers in the SW Pacific rim (e.g. Victoria Veins-Far    Southeast Lepanto, Philippines); they have also been recognized in the    Andes of South America, North America and in the Carpathian Mountains    (Western Tethyan) of Eastern Europe.--  The Tulare Copper-Gold Porphyry Project is located in southern Serbia,    approximately 230 km from Belgrade and 70 km from the regional centre of    Nis. Access to the project is excellent via sealed roads. A rail heading    is available some 45 km from the project area at the city of Leskovac,    or 30 km to the northwest at the town of Kursumlija. Reticulated power    passes close to the project area.--  The Tulare Copper-Gold Porphyry Project area lies within the Lece    Volcanic Complex of southern Serbia; the second largest magmatic complex    in Serbia after the Timok Magmatic Complex.--  Preliminary metallurgical test work on diamond drill core samples from    Bakrenjaca will be selected and dispatched during Q1 2013.--  Dunav plans to commence a detailed drill assessment of the Bakrenjaca    target area during the first half of 2013 in order to determine the    potential mineralized footprint of that epithermal system.6.  SAMPLING AND ANALYSIS

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