Gelum Resources Corp. reported that all results have been received for the geochemical sampling programme carried out in September this year on the Eldorado Gold Property, located within the Bralorne-Bridge River Gold District in south-central British Columbia. The results confirm and significantly expand some of the historical gold anomalies generated by previous workers. The Eldorado Gold Property is located 22 kilometres north of the Bralorne mine, and 17 kilometres North of the community of Gold Bridge. The 9028-hectare property covers multiple Minfile listings and two past-producing, small-scale gold mines that form the northern extent of the Bridge River-Bralorne/Pioneer orogenic gold system. Gold occurs in polymetallic sulphide veins and vein stockworks within broad quartz-carbonate alteration in the Eldorado granodiorite stock and surrounding rocks. These units are complexly juxtaposed along numerous faults associated with regional-scale structures linked to gold mineralization in the region. Gelum collected 62 continuous chip rock samples over several exploration targets, and 485 soil samples from lines over the extensive serpentinite & listwanite alteration west of the Northern Lights and Lucky Strike workings. Additional ridge crest soil lines were completed north of Lucky Jem, on the north-facing slope at the headwaters of Nea Creek (historically sluiced for gold), and both sides of Nea Peak filling gaps in historical soil grids. The Northern Lights soil and rock gold anomaly is currently considered a first-order drill target. Gelum's soil grid extended the gold soil anomaly an additional 500 metres to the south of a grid completed by Gold Fields in 2011. Peak soil values occur between the two Northern Lights adits, with a maximum value of 2.76 g/t Au; some of this mineralization may be dispersal from historical workings in the area. The source of the gold appears to be extensive listwanite (iron carbonate) alteration within volcanic, sedimentary, and ultramafic rocks below a gently east- dipping sill of Eldorado pluton diorite. Above this sill and structurally under a gabbro unit there is a 10-15m thick, east-dipping iron carbonate, which was rock sampled in detail and had the highest, most consistent antimony values of the programme, associated with gold up to 0.214 g/t. The northern extent of this layer at depth is another target (Taylor). The rock sampling also focused on the extensive rock exposure in the north-facing cliff below Nea Peak, where east-dipping, closely spaced, 1-3m thick iron carbonate veins cut the Eldorado diorite. These units have variable gold values (many in the 0.1-0.2 g/t over 1-2m, the higher at 1.4 g/t over 3m), but more consistent arsenic and antimony values, which are pathfinder elements in the Bralorne area.