Zenith Minerals Limited announced four new drill targets have been defined by recent geophysical surveys at the Develin Creek copper-zinc massive sulphide project in Queensland. The new drill targets were identified by induced polarisation (IP) geophysical surveys carried out at the Snook and Wilsons copper-zinc prospects and comprise: Two new high-quality drill targets identified at Snook (S1 & S2) located 30km south of the existing resource area and beneath and adjacent to recent Zenith drilling that has intersected massive copper-zinc sulphides an two new high conviction targets beneath shallow soil cover and along strike of surface gossans at the Wilsons prospects (W1 & W2). The IP geophysical technique is typically used to detect subsurface accumulations of disseminated sulphides that in the case of the Develin Creek type copper-zinc deposits form a broad halo below the massive sulphide copper-zinc deposits. A total of eight copper-zinc targets are now ready for drill testing, these include the four IP targets at Snook and Wilsons and four additional targets located close to the existing Sulphide City JORC copper-zinc sulphide deposits. The latter were defined by a reinterpretation of geology, geochemistry and airborne electromagnetic survey (EM) data. Assays are anticipated shortly from the recent Sulphide City diamond drill twin hole program which was designed to assess potential copper-zinc grade "under-call" associated with historic open hole percussion drilling. Diamond core from the program will also provide suitable sample material for metallurgical testwork. This work is to commence in early July 2021. The Develin Creek project contains a VMS copper-zinc deposit with an Inferred Mineral Resource (JORC 2012) of: 2.57Mt @ 1.76% copper, 2.01% zinc, 0.24g/t gold and 9.6g/t silver (2.62% CuEq) released to ASX on 15-Feb-2015. Zenith's technical team outlined the Snook target located 30km south of the existing JORC resources (Figure 1). An initial maiden drill test of 7 shallow RC holes has been a success, with hole ZSRC001 intersecting 3m of massive and semi-massive sulphides close to surface, at a depth of only 20m downhole. This zone returned: 3m @ 1.57% Cu, 1.07% Zn, 0.37% Pb, 43 g/t Ag and 0.2g/t Au, including 2m of massive sulphide grading: 1.95% Cu, 1.34% Zn, 0.48% Pb, 55 g/t Ag and 0.3g/t Au, within a broader interval of disseminated and stockwork sulphides assaying 12m @ 0.81% Cu, 0.56% Zn. 0.19% Pb, 22g/t Ag & 0.1 g/t Au. Additional RC drill holes (ZSRC002 to ZSRC007) all intersected anomalous levels of copper, zinc and lead as well as precious metals and trace elements, including 1m @ 0.63 g/t Au, 21 g/t Ag, 0.08% Cu, 0.34% Pb, 0.01% Zn in ZSRC005 from 3m below surface. Drilling and mapping have outlined a 200m long zone, now interpreted to be a sub-vertical fault structure cutting the flat lying to gently east dipping host rock sequence. A further two short diamond drill holes (ZSDD001 & 002) were subsequently completed close to hole ZSRC001 to obtain core of the massive sulphides and confirm the shallow dip of the sedimentary host sequence at Snook. ZSDD001 returned 0.3m @ 1.5% Cu, 1.8% Zn, 0.5%Pb, 0.2g/t Ag & 65.2g/t Au associated with a narrow band of massive sulphide, whilst hole ZSDD002 intersected dolerite in the massive sulphide target zone. The IP survey results show a small coincident chargeability high associated with the Snook massive sulphide zone with a deeper much stronger IP target lying beneath the current drilling and another strong target to the east. A dipole-dipole IP survey (DDIP) consisting of 3 trial survey lines at Snook was completed with the aim of identifying zones of disseminated sulphide mineralisation that typically form as a halo or "feeder zones" beneath volcanic hosted massive copper-zinc sulphide deposits. The survey was successful in identifying several strong chargeability anomalies up to 40mv/V in areas of high resistivity consistent with disseminated sulphides within the basalt host rock target sequence below a sedimentary unit (zone of low resistivity). These targets (S1 & S2) lie below the existing drill holes that contained strongly anomalous copper-lead-zinc and precious metals and will be tested by a series of up to 7 drill holes. The IP anomaly remains open to the south providing further upside. In addition, a DDIP survey consisting of 7 survey lines was completed at the Wilsons prospect extending north. A strong chargeable anomaly coincident with a resistive high (inferred basalt host sequence) was defined beneath the target area that is obscured by soil. Like Snook, the Wilsons drill targets (W1 & W2) are consistent with a zone of sub-surface disseminated sulphides that typically form as a halo or "feeder zones" beneath volcanic hosted massive copper-zinc sulphide deposits. Two to three drill holes are planned to test the Wilsons IP targets.