Consolidated Zinc Limited announced that high-grade gold mineralisation has been confirmed at its 100% owned Plomosas concessions, located to the north-west of the current zinc-lead-silver mining operations at Plomosas, operated by CZL's wholly owned subsidiary, Minera Latin American Zinc S.A.P.I de C.V. (MLAZ) Geological mapping of the sequence trending to the north-west of the Plomosas zinc-lead-silver mine has identified what appears to be an additional gold mineralised system. First pass rock chip results of outcrops and old workings returned exciting results with grades up to 61.0g/t Au, 27.5g/t Au and 7.42g/t Au. The system is defined by complex, kilometre-scale geological structures associated with several geophysical anomalies and mineralised outcrops and workings. Historical small-scale mining of high-grade gold and copper quartz veins was undertaken but there have been no previous modern gold exploration methods completed within the Plomosas concessions to assess the implication or potential of these occurrences. Consequently, these results are very encouraging. The rock chip results, indicate identification of a potential gold system over an area of at least one kilometre (1km) within the Plomosas concessions. This will be followed up with an aggressive exploration program to define targets. Mapping and sampling are currently ongoing, and results will be made announced as received. Chona and Enrique Vein Systems Located approximately 5km to the west-northwest of Plomosas zinc-lead-silver mine and within the Don Lucas concession, the Chona and Enrique mineralisation occur as thin veins developing to wider zones of mineralisation, interpreted to be mesothermal in origin. Veins in the immediate Chona area are typically around 20-30cm in thickness, however previous reports have noted veins up to 1.2 metres thick, with a visual strike extent of around 100 metres with a dip of 80O and strike of 330O. Veins are granular, containing quartz, carbonate and haematite as gangue to malachite at around 3%. Zonation in the veins show a malachite centre with haematite rims and edges. The Chona veins have previously been worked by locals, creating a strike drive from which around 1,200 tonnes (field estimation only) was removed. Historical assay values from Chona include 8.37g/t Au, 2.45% Cu (Schultz, 2006), 10.4g/t Au, 5.18% Cu (Goodell 2009), 11.23g/t Au, 6.0% Cu (Secretaria de Desarrollo Industrial, 2008) and 0.877g/t Au, 17.1% Cu, (Laforest 2010). The Enrique veins are interpreted to be the continuation of the Chona veins system and are located 420 metres further to the northwest. Enrique is a thicker vein system, can be traced on surface for around 60 metres, varies from 1.5 to 3 metres in thickness and is similar mineralogy to the Chona vein. The veins dip 65O to the north east with a strike of around 345O. There is potential for the gold bearing veins to swell, narrow and cluster along strike. Historic assays from Enrique are 21.3g/t Au and 2% Cu, (Goodell, 2008). MLAZ samples collected from Chona returned values of: 61.0g/t Au, 6.9g/t Ag, 2.88% Cu (sample 38161); 27.5g/t Au, 4.1g/t Ag, 2.19% Cu (sample 38160); 7.42g/t Au, 4.2g/t Ag, 2.91% Cu (sample 38162); and 4.77g/t Au, 3.8g/t Ag, 4.06% Cu (sample 38158). These areas are considered highly prospective and will be assessed further during the 2020 exploration year. TMI 1VD air magnetics in the Don Lucas area shows several linear blocks defined by strong northwest structures. Along one of these northwest lineaments occur the mineralisation that is Chona and Enrique veins.