Azure Minerals Limited confirmed that massive, semi-massive and matrix sulphide mineralisation intersected in drill holes ANDD0005 and ANDD0006 at the Andover Ni-Cu Project (60% Azure /40% Creasy Group) returned significant nickel and copper assays within broad mineralised envelopes. Holes ANDD0004, 0005 and 0006 combine to define a vertical mineralised section exceeding 120m, with the nickel-copper mineralisation remaining open in both up-dip and down-dip directions, as well as along-strike to the east and west. Azure has completed seven diamond drill holes for a total of 2,720m at the Andover Ni-Cu Project. Importantly, all seven holes have intersected broad mineralised intervals containing substantial nickel-copper sulphide mineralisation. In every hole massive sulphide zones coincide with strong electromagnetic conductors detected by surface fixed-loop electromagnetic (FLTEM) surveys and subsequently confirmed by down-hole (DHTEM) surveys. Geological logging and assay results confirm that this nickel-copper sulphide mineralisation is clearly associated with the strong, large and continuous VC-07 EM conductor. Geophysical modelling indicates that VC-07 extends for at least 1,050m to the west-northwest and has a potential depth extent exceeding 150m-200m. ANDD0005 and ANDD0006: ANDD0005 and ANDD0006 were drilled to test the up-dip and down-dip extensions of the 38m-wide zone of nickel-copper sulphide mineralisation intersected in ANDD0004, which returned 16.2m (estimated true width 10.1m) @ 2.09% Ni and 0.75% Cu from 347.5m in the eastern part of the extensive (1,050m x +200m) VC-07 conductor, identified by Azure in electromagnetic surveys. ANDD0005 returned mineralised assays over an 18.7m-wide (estimated true width 15.4m) mineralized interval, containing significant quantities of nickel and copper sulphide mineralisation in the form of massive, semi-massive, matrix, blebby and disseminated nickel-copper sulphide mineralisation hosted in gabbro and other mafic rocks. ANDD0006 intersected a broad 47.5m-wide (estimated true width 25.0m) mineralised envelope, containing multiple intervals of strong nickel-copper sulphide mineralisation approximately 60m down-dip from ANDD0004. The mineralised envelope includes significant intervals of massive, matrix and disseminated nickel-copper sulphide mineralisation hosted in gabbro and other mafic rocks. Holes ANDD0004, 0005 and 0006 define continuity of high-grade nickel-copper sulphide mineralization over a down-dip extent exceeding 120m, with the mineralisation remaining open both up and down-dip from these intersections. DHTEM surveying in ANDD0006 highlighted strong conductivity coincident with the intersected massive sulphides and modelling indicates that mineralisation extends for a significant distance down-dip below the hole.