Carawine Resources Limited announced new assay results from seven RC holes, and visual results from four diamond drill holes, completed as part of an expanded 33-hole follow-up drilling program at the Hercules prospect. Assay results reported are from RC drill holes TNRC026 to TNRC032, which targeted mineralization near the base of cover and in the northern extent of the deposit. Visual results from diamond drill holes TNDD002 to TNDD005 are also reported, including a 4.3m-wide (downhole) laminated sulphidic quartz vein typically associated with the Hercules mineralisation intersected in TNDD005 at approximately 250m from surface. Assays results for five completed diamond holes, and a further three RC holes are pending, with at least 16 additional diamond holes planned to come in the current, expanded program. Hercules is an advanced gold prospect held by Carawine's Thunderstruck Joint Venture, which forms part of the Company's large Tropicana North Project located in the north-eastern goldfields of Western Australia. The current follow-up drilling program comprises 33 planned holes, of which 17 have been completed to date (12 RC and five diamond holes), and is designed to test mineralisation over more than 400m of strike and 200m length down-dip. The current Hercules drilling program is focussed on defining and extending gold mineralization associated with the mineralised structures and the multiple lodes intersected in drilling to date. These include the exceptional high-grade results returned from Carawine's initial round of drilling completed earlier this year, and positive results received from the current program. RC Assay Results: Significant intervals (above 0.3g/t Au cut-off) reported from RC drill holes TNRC026 to TNRC032 are listed as follows: 2m @ 6.76g/t Au from 141m (0.3g/t Au cut-off) (TNRC032) including: 1m @ 13.2g/t Au from 141m (1g/t Au cut-off); and 2m @ 0.80g/t Au from 157m (0.3g/t Au cut-off); 2m @ 0.86g/t Au from 111m (0.3g/t Au cut-off) (TNRC031); including 1m @ 1.24g/t Au from 111m (1g/t Au cut-off); and, 1m @ 0.74g/t Au from 117m (0.3g/t Au cut-off); and 1m @ 1.07g/t Au from 121m (0.3g/t Au cut-off); and 1m @ 0.96g/t Au from 139m (0.3g/t Au cut-off) (main trend); 1m @ 0.46g/t Au from 73m (0.3g/t Au cut-off) (TNRC030); 1m @ 0.34g/t Au from 87m (0.3g/t Au cut-off) (TNRC026); and 1m @ 0.70g/t Au from 167m (0.3g/t Au cut-off). The high-grade interval in TNRC032 of 1m @ 13.2g/t Au from 141m is associated with a sheared, strongly chloritic monzonite and correlates well with mineralisation 40m up-dip in TNRC009, which returned 5m @ 10.0g/t Au from 85m (0.3g/t Au cut-off). This result expands the high grade (> 10 gram-metres) zone this area of the prospect. TNRC031 intersected low-grade gold at the targeted main trend position (1m @ 0.96g/t Au from 139m). From 111m to 121m - above and to the southeast of the main trend - a broad zone of semi-massive sulphide (pyrite-dominant) was intersected, returning a number of anomalous gold intervals ranging from 0.74g/t Au to 1.24g/t Au. This varies from the laminated sulphidic quartz veining associated with the main mineralised trend at Hercules and may represent a new target requiring further drilling. TNRC026 intersected sulphidic quartz veins approximately 35m up-dip from the high-grade intercept in TNRC010, and although returning low gold grades, demonstrates the continuity of the structure through this area. TNRC027 to TNRC029 did not intersect the targeted structure or mineralisation, and TNRC030 lifted considerably from design, intersecting the target zone about 20m below historic drill hole NLC128. Diamond Core Visual Results: Laminated sulphidic quartz veins intersected at target depths have been logged and sampled in three of the five diamond drill holes completed to date. TNDD001, reported previously, has visible gold within sulphidic laminated quartz veins from 166.68m to 167.12m and 169.03m to 169.77m downhole. Similar veining was logged in TNDD005 from 281.4 to 285.7m downhole, and in TNDD002 from 60.3 to 60.98m downhole at the start of a ~44m interval of monzonite and multiple, narrow sulphidic quartz veins between 60.3m and 104.05m. The veining in TNDD005 extends the main structural zone to at least 250m below surface (220m below the base of cover), with the potential to extend the main mineralised zone once assay results are received. TNDD003 intersected a strong, pyritic chlorite/carbonate shear zone between 273.5 and 274m downhole at the targeted depth, with additional sulphidic breccia zones also intersected further downhole between 291.8m and 295.5m.