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RAMELIUS RESOURCES LIMITED — Capital/Financing Update 2004
Nov 7, 2004
65718_rns_2004-11-07_7c5a95b0-e19a-48b7-83c5-a7934bc9b452.pdf
Capital/Financing Update
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Ramelius Resources Limited
RAMELIU
ACN 001 717 540
140 Greenhill Road, Unlev SA 5061 GPO Box 1373, Adelaide SA 5001 DX 52003, Unlev Telephone (08) 8373 6473 or (08) 8373 5588 Facsimile (08) 8373 5917
ASX RELEASE
For Immediate Release 8 November 2004
General Manager The Company Announcements Office Australian Stock Exchange Limited PO Box H224 Australia Square Sydney NSW 1215
Dear Sir/Madam,
HILDITCH NICKEL EXPLORATION UPDATE
HIGHLIGHTS
- Drilling identified two zones of nickel and copper mineralisation.
- Two additional areas of nickel gossans identified.
OUTLOOK
- Further drilling is planned to follow up the mineralised intersections in drill holes HRC 01, 02, and 03.
- Similarly, geochemical drilling will be undertaken to test the additional areas of identified nickel gossans.
SUMMARY
Nickel sulphide exploration continued at the Company's Hilditch tenements with:
- Further gossans which exhibit the geochemistry expected in nickel sulphide gossans being identified in the southern central sector of the tenements,
- Geochemical drill testing of the gossans identified in the north eastern corner of the tenements, which returned encouraging results in three holes.
Drill testing of the identified Gossans
A total of 974m in 24 reverse circulation holes were drilled in the north eastern corner of the tenements below gossans that had been identified as being after nickel sulphides. The cuttings were analysed for nickel, copper, cobalt and several other elements that are useful in determining geological and geochemical relationships. Selected intervals are yet to be submitted for platinum, palladium and gold analysis.
The geochemical drilling used the RC drilling method and a three hole scissor pattern where, because of structural uncertainty as to the dip direction of the target horizon below the gossan, the holes are drilled from either side of the gossan so as to cross at depths of approximately 15 m and 25m below the dossan.
The location of the drilled gossans is shown on the accompanying map.
Drill holes HRC001 to HRC003 at the northern most gossan location returned the most encouraging results intersecting two nickel and copper enriched zones on the contact of ultramafic rocks against sediments and sheared mafic rocks.
| Hole No | North (GDA) |
East (GDA) |
Azimuth | Dip | From $ $ | To | Length | Ni% | Cu% |
|---|---|---|---|---|---|---|---|---|---|
| HRC001 | 6537111 | 355179 | 270 | $-60$ | 33 | 35 | $2^{\star}$ | 0.70 | 0.18 |
| HRC002 | 6537111 | 355154 | 90 | -60 | 3 | $2**$ | 1.20 | 0.53 | |
| HRC003 | 6537111 | 355144 | 90 | $-60$ | 17 | 19 | $2**$ | 0.67 | 0.08 |
| and | 34 | 36 | $2^*$ | 0.41 | 0.07 |
These results are tabulated below.
eastern zone, intersected as the scissor holes crossed.
western zone.
Further drilling is to be undertaken to test these mineralised horizons below the current drilling and along strike.
Drilling on the gossans further to the south (refer to the accompanying map) has confirmed that the gossan locations are within the ultramafic sequence, probably on "interflow interfaces". Some horizons within the ultramafic sequence show elevated copper geochemistry that may correlate with the gossans. These intervals are yet to be analysed for platinum, palladium and gold, elements that may help identify mineralised horizons.
The southern most drilling was centred on a strongly outcropping gossan. There is no specific geological feature evident in the drilling to correlate with the gossan; however a mafic unit, thought to be an intrusive was intersected in all three holes at the interpreted position of the gossan horizon. It is possible that
the intrusive has stoped out the prospective horizon and additional drilling is planned for this location.
Two additional Gossan zones identified
Two areas of gossanous ironstone that exhibit the geochemistry of nickel sulphide gossans have been located in the southern central area of the tenements. The northern most of these areas contains gossans in outcrop while in the southern area the gossans are recorded as scree.
The following table shows the geochemistry of some of these gossans.
| Sample | Co-ordinates | Cu | Ni | Pd | Pt | $\mathbf{z}_n$ | |
|---|---|---|---|---|---|---|---|
| No | East | North | ppm | ppm | ppb | ppb | ppm |
| HR162 | 355404 | 6535062 | 1501 | 8169 | 107 | 82 | 217 |
| HR145 | 355371 | 6535585 | 1592 | 12669 | 722 | 410 | 27 |
| HR143 | 355368 | 6535594 | 1215 | 13082 | 156 | 241 | 50 |
| HR144 | 355365 | 6535599 | 1035 | 6121 | 108 | 113 | 222 |
| HR133 | 355354 | 6535645 | 1431 | 12261 | 2594 | 70 | 830 |
| HR123 | 355301 | 6535811 | 1232 | 2490 | 421 | 225 | 834 |
| HR117 | 355316 | 6535863 | 429 | 2031 | 35 | 40 | 107 |
At these locations it is proposed to geologically map the areas, undertake additional rock chip sampling, as necessary, ahead of a similar geochemical drilling programme to that undertaken in the north eastern sector.
For further information please contact:
Mr. Joe Houldsworth Managing Director Ramelius Resources Limited Ph. 08 9250 6644
