European Metals “Two excellent drill holes in terms of Lithium grade and length” says CEO Keith Coughlan

European Metals LON:EMH CEO Keith Coughlan said: “I am pleased to report results from two additional drillholes from the recently completed drilling program at Cinovec Main. These results are excellent in terms of lithium grades and length of mineralised intervals. An unexpected bonus is a high-grade zone of tungsten, intersected by drillhole CIW-22 at 238 meters depth which graded almost 3% of tungsten.

In addition, we are pleased to have been informed that subsequent to a submission we made to the State Authority, the Cinovec South resource estimate was approved by a Committee of Experts and placed on the State Register of mineral deposits. This is a pre-requisite for receiving a mining permit. We already applied for the ‘preliminary mining space’ for Cinovec South, immediately after the resource calculation for Cinovec South was accepted to the State Register.”

European Metals Holdings Limited has given DirectorsTalk analytical results for two drillholes from the recently completed drilling in the Cinovec Main sector of the deposit. These results confirmed or exceeded the expected lithium content and mineralisation widths.

In addition, the Cinovec South Resource has now been added to the Czech State resource register. This is the first step in the process for the granting of a mining permit.

Key Points:

 
 
        *    Hole CIW-22 contains the best lithium intercept 
             to-date from the Company's drill programme of 264.5 m 
             averaging 0.54% Li(2) O. 
 
        *    This hole also contains significant tungsten, tin, 
             niobium and tantalum mineralization. For example, the 
             best interval between 238m to 240m averages 0.86% 
             Li(2) O, 0.41% Sn, 2.92% W, 868ppm Nb, 150ppm Ta. The 
             tungsten grade in particular was significantly higher 
             than expected. 
 
        *    Hole CIW-26 returned an interval of 236.25m averaging 
             0.49%Li(2) O (including high-grade intervals 
             16m@0.99%Li(2) O, 3m@1.15% Li(2) O, 2m@1.34% Li(2) O, 
             2m@0.99% Li(2) O, 1.3m@1.72% Li(2) O, 2m@0.93% Li(2) 
             O, 5m@0.84% Li(2) O. 
 
        *    Drillhole CIW-26 is located at the western edge of 
             the deposit near the contact of the mineralisation. 
             Drillhole CIW-22 is located in the central part of 
             Cinovec Main. 
 
        *    All remaining analytical results from the program 
             will be released next week. 
 
        *    Geological information from all 17 drillholes has 
             been compiled into the Cinovec database and serves to 
             update the geological model for Cinovec Main. The 
             geologic model will be used to constrain and update 
             the current block model. The block model will be 
             updated in early February when all analyses will be 
             available. The block model and resource calculation 
             will be part of the Pre-Feasibility Study. 

 

Drill Programme

The CIW-22 was collared in the central part of Cinovec main, whereas drillhole CIW-26 was located at the western edge of the Cinovec Main sector of the deposit (see Figure 1).

The current drill programme at Cinovec Main has been planned to confirm and delineate near surface lithium and tin mineralisation that would provide initial feed to the mill. Other goals are the conversion of resources from the Inferred to Indicated category, and delivery of material for metallurgical testing. 17 diamond core holes have been completed. Visual inspection and logging indicates that the geology in these holes is as expected. Drill details are listed in Table 1 below.

After geological logging, drill core is cut by a diamond saw. Quarter core samples are selected (honouring geological boundaries) and dispatched to ALS (Romania) for preparation and assay; the 3/4 of the core is returned to the core box and stored securely on site. Samples are being prepared and analysed by ALS using ICP and XRF techniques following standard industry practice for lithium and tin deposits. Strict QAQC protocols are observed, including the insertion of a Li standard in random fashion for every 10 core samples, as well as the insertion of blank and duplicate samples.

Table showing the completed drillholes, Cinovec Main

 
  Hole       North         East      Elevation   Depth   Azimuth    Dip          Comments 
    ID                                  (m)       (m) 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-11    -779299.50   -966097.50    867.40     444.4    40.10    -77.86   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-20    -778810.50   -965638.00    837.50     257.6   336.70    -84.60   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-13    -779175.50   -966126.84    862.80     429.3    76.00    -80.40   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-19    -778810.80   -965692.10    837.80     271.6   332.10    -89.58   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-08    -778791.39   -965800.23    837.60     274.9   156.85    -89.30   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-18    -779018.59   -966182.61    855.47     395.7   210.60    -89.05   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-14    -779055.85   -966093.30    854.46     417.8   323.30    -89.07   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-07    -778867.31   -965841.48    840.99     300.0   333.60    -89.57   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-26    -779214.82   -965937.24    865.33     430.5   248.00    -89.38   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-17    -778957.07   -965520.58    847.07     238.2   332.10    -89.58   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-21    -778811.80   -965952.31    841.33     320.6    42.68    -89.02   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-10    -779215.43   -965938.41    865.35     455.0   303.40    -74.47   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-23    -779008.92   -965993.87    848.91     376.1   222.30    -89.40   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-22    -779009.34   -965993.42    848.88     420.6   287.90    -70.43   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-06    -778995.26   -965844.93    846.77     296.3    11.70    -80.18   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-25    -778994.45   -965901.56    847.04     382.4   281.10    -69.89   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 
 CIW-27    -779152.42   -965816.56    861.50     370.0   271.90    -89.53   confirmation/infill 
--------  -----------  -----------  ----------  ------  --------  -------  -------------------- 

Hole locations are recorded in the local S-JTSK Krovak grid, all coordinates are surveyed.

Mineralised Intercepts and Lithology

The drillhole CIW-26 was located near the granite-porphyry contact, testing lithium mineralisation near the western edge of the deposit. In this location, at the W and NW part of the deposit, the contact is relatively steeply dipping. The CIW-26 drillhole was drilled from the same site as CIW-10 but was vertical.

The drillhole CIW-22 was collared in the central part of the Cinovec-Main deposit where the Cinovec lithium granite daylights, drilled from the same site as CIW-23. CIW-22 was angled -70degree toward West (288 degrees).

CIW-26 started in the overlying barren porphyry. The porphyry-granite contact at 174m drill string depth (DSD) is of tectonic nature. Immediately below the contact a massive greisen was intersected to DSD of 203 meters. The interval between 203m to 296m DSD is dominated by albite granite with zinnwaldite, locally including zones of greisenized granite and greisen. Below, down to DSD of 424m, is a long zone of greisenized granite, underlying by low-mica weakly mineralised granite that forms the base of the lithium mineralization. In CIW-26, very few core angles of contacts were observed. A narrow greisen contact was measured at 27 degrees, and as the core was not oriented, it is impossible to ascertain with certainty the orientation of the mineralised zones. Therefore, the mineralised intercept may not represent true width. The geological model predicts that at the western contact the greisen dip W.

Drillhole CIW-22 starts in granite to DSD of 124m. Interval between 124 and 182m is formed by greisen and greisenised granite, locally with quartz veins. One wider stope after historic mining was intersected. A long interval formed mostly by greisenised granite was intersected between 205m and 382m, confirming the general paradigm of two major greisen zones separated by albite-zinnwaldite granite. The base of the hole is low-mica granite. As usual the contacts are mostly gradational. Core angles of sharper contact are steep at around 60 degrees so the intercept lengths do not represent true widths of mineralisation but are likely reasonably close based on the general geological model. At 238 meters an unusually high grade zone of tungsten was intersected. This interval is formed by a quartz-zinnwaldite greisen with crystals of wolframite, with greisenized granite footwall and hanging wall. Due to relative lack of data is it difficult to assess the orientation of this high grade zone at this time.

The Tables below list the mineralised intercepts for the two drillholes.

Table summarizing mineralised intercepts in CIW-22

 
                                    CIW-22 
 From     To     Interval   Li(2)     Sn    W (%)             Note 
                    (m)      O (%)    (%) 
  10      28        18       0.22 
  100     119       19       0.21 
                                                       incl. 6m@1.17%Li2O 
                                                         (129.5-135.5m), 
                                                     4m@0.92%Li2O (141-145m), 
                                                     7m@0.91%Li2O (175-182m), 
  123    387.5    264.5      0.54                    2m@1.07%Li2O (256-258m) 
  125    134.5     9.5       0.96    0.22   0.071 
 128.5   135.5      7        1.12    0.25   0.095 
  141     143       2        1.25    0.07   0.408 
  160     161       1        0.71    0.02   0.157 
  167     168       1        0.93    0.20   0.046 
  175     179       4        0.98    0.01   0.091 
  234     235       1        0.48    0.03   0.059 
                                                        868ppm Nb, 150ppm 
  238     240       2        0.86    0.41   2.915               Ta 
  256     257       1        1.16    0.02   0.070 
  221     252       31                                      150ppm Nb 
  286     331       45                                      104ppm Nb 
------  ------  ---------  -------  -----  ------  -------------------------- 
   Cut-off: 0.2%Li(2) O, 0.1%Sn, 0.05%W, determining 
    metal for definition of interval in bold 

Table summarizing mineralised intercepts in CIW-26

 
                                       CIW-26 
  From     To     Interval   Li(2)     Sn    W (%)                Note 
                     (m)      O (%)    (%) 
                                                           incl. 16m@0.99%Li2O 
                                                               (186-202m), 
                                                         3m@1.15%Li2O (186-189m), 
                                                         2m@1.34%Li2O (192-194m), 
                                                         2m@0.99%Li2O (246-248m), 
                                                      1.3m@1.72%Li2O (253.1-254.4m), 
                                                         2m@0.93%Li2O (308-310m), 
 173.75    410     236.25     0.49                       5m@0.84%Li2O (369-374m) 
  178      181       3        0.70    0.01   0.111 
  187      188       1        0.84    0.11   0.003 
 346       368       22       0.45                              103ppm Nb 
 379      423.5     44.5      0.26                              111ppm Nb 
-------  ------  ---------  -------  -----  ------  -------------------------------- 
   Cut-off: 0.2%Li2O, 0.1%Sn, 0.05%W, determining 
    metal for definition of interval in bold 

(Please refer to the announcement on the European Metals Website for the graphic Figure 1 – A geological map showing the Company’s drill holes (with angled holes traces projected to surface) against surface geology and subsurface greisen bodies projected to surface (in green). Historic UG workings and drill holes not shown – www.europeanmet.com.)

CINOVEC SOUTH RESOURCE ADDED TO CZECH STATE RESOURCE REGISTER

The process for the award of a mining permit commences with the placing of a mineral resource on the State Resource Registry and receiving a certificate of an ‘exclusive mineral deposit’. This is achieved by defending a resource calculation and a preliminary technical and economic analysis proving the studied resource has a quality consistent with a potentially mined deposit. The addition to the State Resource Register means that civic development on top of the area is restricted and it allows the Company to apply for a setting a preliminary mining space, which is a step toward obtaining the final mining permit.

The company is currently working on the submission for the remaining NW part of the orebody and on placing it on the State Resource Registry.

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