Dacian Gold Limited announce exploration drilling results at the Jupiter mining complex below the Heffernans and Ganymede open pits, located at its Mt Morgans Gold Operation (MMGO). These results have intersected mineralisation at depth in the Jupiter syenite intrusive system, at the limit of, and below the Mineral Resource estimate. The Jupiter syenite intrusive complex spans a north south extent of approximately 2km with variable width ranging between 50m to 300m. The exploration program is continuing with the first four holes now completed into Heffernans and Ganymede, and the drilling of an additional seven holes at Heffernans is currently underway. The current Mineral Resource for the Jupiter mining area totals 14.6Mt at 1.3g/t for 599,000oz. These drilling results are outside the current Mineral Resource boundary at Ganymede and within the inferred Mineral Resource at Heffernans. Heffernans Drilling Results Diamond drilling designed to test for mineralisation and structural orientation, intersected wide zones of mineralisation in 21JUDD0812, within syenite and basalt. Recent geological studies resulted in a change to drill orientation of 21JUDD0811W1 compared to historical drilling, with the successful result representing an important change in the approach to design for exploration drilling and modelling. Significant high-grade intersections below the Heffernans open pit included key intercepts of: For hole 21JUDD0811W1, 102.9m @ 1.4g/t from 436.3m, including: o 14.7m @ 7.2g/t Au from 467.9m o 2.7m @ 2.7g/t Au from 501.2m o 1.4m @ 4.6g/t Au from 514.5m For hole 21JUDD0812: o 5.1m @ 1.3g/t Au from 241.4m, o 0.6m @ 12.5g/t Au from 263.0m, o 2.5m @ 2.2g/t Au from 404.0m, o 8.0m @ 1.4g/t Au from 415.0m, o 8.7m @ 1.6g/t Au from 497.0m, o 11.4m @ 1.2g/t Au from 557.6m, o 22.4m @ 1.0g/t Au from 599.6m, o 2.7m @ 5.7g/t Au from 765.0m, Ganymede Drilling Results The Ganymede syenite is located immediately south-west of Heffernans, separated by an east-west oriented felsic porphyry intrusive. Mineralisation at Ganymede is observed as stockwork style along the syenite basalt contact and along interpreted structural planes through the syenite. This style of stockwork mineralisation has been intersected in the two completed drillholes. There is a north-south oriented hole planned in the current program to test for existing and alternate structural control on mineralisation.