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CULLEN RESOURCES LIMITED — Capital/Financing Update 2007
May 15, 2007
64724_rns_2007-05-15_5859e627-ea7e-4830-aea3-d1f0c1e9076e.pdf
Capital/Financing Update
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Aquila Resources Limited ABN 81 092 002 769
Level 2 Aguila Centre 1 Preston Street Como WA 6152
PO Box 1038 South Perth WA 6951
Telephone: (61) 8 9423 0111 Facsimile: (61) 8 9423 0133 [email protected] www.aquilaresources.com.au
Companies Announcements Office Australian Stock Exchange Limited 4th Floor, 20 Bridge Street SYDNEY NSW 2000
16 May 2007
Initial Corte Resource Estimate for the West 211 and hon Ore Protect totals 265.9 Ml
Aquila Resources Limited ("Aquila") is pleased to announce the results of the initial JORC resource estimate for the Australian Premium Iron Joint Venture ("API"), in which the Company has a fifty percent interest, in relation to its West Pilbara Iron Ore Project located in the Pilbara region of Western Australia.
Golder Associates Pty Ltd was commissioned to complete the in-situ resource estimates.
The West Pilbara Iron Ore Project, located approximately 50 kilometres southwest of Pannawonica in the Pilbara region of Western Australia, has been the major focus of the Company's exploration program since its commencement in 2005. An extensive reverse circulation drilling program completed in 2006 evaluated five Channel Iron Deposits ("CID"), resulting in resource estimates being finalised for the Catho Well, Cardo Bore East, Upper Cane, Jewel and Cochrane CID, which all form part of the West Pilbara Iron Ore Project.
The Catho Well deposit is located in the Mt Stuart Joint Venture area (API 70%, Cullen Resources Limited 30%) whilst the Cardo Bore East, Upper Cane, Jewel and Cochrane deposits are located within the Red Hill Joint Venture (API earning 80%, Red Hill Iron Limited 20%).
The Indicated and Inferred resource for the pisolitic CID of the West Pilbara Iron Ore Project totals 203.0 Mt at 57.44% Fe.
Channel Iron Deposits - West Pilbara Iron Ore Project resource statement (JORC compliant).
| Resource | Tonnage | Average Grade | |||||||
|---|---|---|---|---|---|---|---|---|---|
| Classification | (Mt) | Fe% | SiO 2 % | $Al_2O_3\%$ | Р% | S% | Mn% | MaO% | LOI% |
| Indicated | 47.7 | 55.45 | 6.68 | 3.02 | 0.038 | 0.016 | 0.079 | 0.170 | 10.26 |
| Inferred | 20.3 | 55.23 | 7.15 | 3.24 | 0.037 | 0.016 | 0.071 | 0.161 | 9.83 |
| Total | 68.0 | 55.38 | 6.82 | 3.09 | 0.038 | 0.016 | 0.077 | 0.167 | 10.13 |
Catho Well Deposit (cut-off grade >54% Fe, no Al2O3 cut-off applied)
Cardo Bore East Deposit (cut-off grades >54% Fe and <4.0% Al2O3)
| Resource | Tonnage | Average Grade | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| Classification | (Mt) | Fe% | SiO 2 % | AI 2 O 3 % | P%. | S% | Mn% | MaO% | LOI% | |
| Indicated | 30.6 | 59.32 | 4.60 | 3.43 | 0.076 | 0.016 | 0.065 | 0.109 | 6.59 | |
| Inferred | 4.8 | 58.98 | 4.85 | 3.46 | 0.072 | 0.017 | 0.055 | 0.119 | 6.68 | |
| Total | 35.4 | 59.27 | 4.63 | 3.44 | 0.075 | 0.016 | 0.064 | 0.110 | 6.60 |
Upper Cane Deposit (cut-off grade $>54\%$ Fe, no Al2O3 cut-off applied)
| Resource | Tonnage | Average Grade | |||||||
|---|---|---|---|---|---|---|---|---|---|
| Classification | (Mt) | Fe% | SiO,% | AI 2 O 3 % | P% | $S\%$ | Mn% | MaO% | LOI% |
| Indicated | 27.8 | 58.74 | 4.97 | 2.88 | 0.082 | 0.020 | 0.024 | 0.043 | 7.55 |
| Inferred | 31.5 | 58.76 | 5.02 | 2.98 | 0.075 | 0.019 | 0.021 | 0.050 | 7.50 |
| Total | 59.3 | 58.75 | 5.00 | 2.93 | 0.078 | 0.019 | 0.022 | 0.047 | 7.52 |
Jewel Deposit (cut-off grades $>54\%$ Fe and <4.4% Al2O3)
| Resource | Tonnage | Average Grade | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| Classification | (Mt) | Fe% | SiO 2 % | AI 2 O 3 % | P%. | S% | Mn% | MgO% | LOI% | ||
| Indicated | 14.4 | 56.87 | 5.78 | 3.52 | 0.057 | 0.026 | 0.023 | 0.057 | 8.95 | ||
| I Inferred | 5.3 | 56.80 | 6.05 | 3.62 | 0.066 | 0.025 | 0.027 | 0.056 | 8.59 | ||
| Total | 19.7 | 56.85 | 5.85 | 3.55 | 0.059 | 0.026 | 0.024 | 0.057 | 8.85 |
Cochrane Deposit (cut-off grades $>54\%$ Fe and <4.2% Al2O2)
| Resource | Tonnage | Average Grade | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| Classification | (Mt) | Fe% | SiO 2 % | $Al_2O_3\%$ | Р% | $S\%$ | Mn% | MgO% | LOI% | ||
| Indicated | 20.7 | 57.90 | 5.05 | 3.59 | 0.079 | 0.020 | 0.012 | 0.115 | 7.91 | ||
| Inferred | |||||||||||
| Total | 20.7 | 57.90 | 5.05 | 3.59 | 0.079 | 0.020 | 0.012 | 0.115 | 7.91 |
Total - Channel Iron Deposits
| Resource | Tonnage | Average Grade | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| Classification | (Mt) | Fe% | SiO 2 % | AI 2 O 3 % | P% | $S\%$ | Mn% | MgO% | ∟OI% | ||
| Indicated | 141.2 | 57.44 | 5.56 | 3.22 | 0.063 | 0.018 | 0.050 | 0.112 | 8.45 | ||
| Inferred | 61.9 | 57.45 | 5.79 | 3.16 | 0.062 | 0.018 | 0.041 | 0.092 | 8.30 | ||
| Total | 203.0 | 57.44 | 5.63 | 3.20 | 0.062 | 0.018 | 0.047 | 0.106 | 8.41 |
The resources have similar iron grades to the pisolitic ores mined at Robe River and Yandicoogina, whilst the average alumina $(A2O3)$ grade is at the upper end of the preferred range, noting that there may be the opportunity to beneficiate or blend this resource with lower alumina ores similar to the Upper Cane resource in order to manage potential product specifications.
Hardey Project
The Hardey Bedded Iron Deposit ("BID") is located approximately 50km west northwest of the township of Paraburdoo in the Pilbara and approximately 130km from the Catho Well deposit.
The Hardey project was identified as potentially hosting a significant BID following a mapping and sampling program completed in early 2006. Reverse circulation drilling has been completed on the major mineralized zones hosted within the Dales Gorge Member of the Brockman Formation and the Nammuldi Member of the Marra Mamba Formation. The mineralised zones are hosted within the eastern fold closure of the Hardey Syncline. The hematite/hematite-geothite mineralisation in the Dales Gorge Member is up to 150m thick at the fold axis and typically 30-40m thick on the southern and northern limbs. A major zone of Marra Mamba mineralisation located on the southern limb of the syncline is a tabular zone approximately 30m thick with a strike extent of 900 metres.
The Indicated and Inferred resource for the Hardey BID is 62.9 Mt at 61.33% Fe.
Hardev Bedded Iron Deposit resource statement (JORC compliant).
| FRATURY DROUSIL (CUL-OIL ULBUR 70076 FR) | |||||||||
|---|---|---|---|---|---|---|---|---|---|
| Resource | Tonnage | Average Grade | |||||||
| Classification | (Mt) | Fe% | SiO2% | AI2O3% | Р% | S% | Mn% | MgO% | LOI% |
| Indicated | 19.8 | 61.24 | 3.66 | 2.66 | 0.128 | 0.011 | 0.063 | 0.069 | 5.69 |
| Inferred | 43.1 | 61.38 | 3.82 | 2.44 | 0.123 | 0.010 | 0.061 | 0.088 | 5.56 |
| Total | 62.9 | 61.33 | 3.77 | 2.51 | 0.125 | 0.010 | 0.062 | 0.082 | 5.60 |
Hardey Danasit (out off grade \£99/ Ea)
| Formation/ | Resource | Average Grade Tonnage |
||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| Domain | Classification | (Mt) | Fe% | SiO 2 % | $Al_2O_3\%$ | P% | S% | Mn% | MaO% | LOI% |
| Brockman | Indicated | 15.5 | 61.58 | 3.34 | 2.71 | 0.146 | 0.006 | 0.071 | 0.060 | 5.49 |
| Inferred | 36.8 | 61.63 | 3.68 | 2.45 | 0.133 | 0.009 | 0.065 | 0.069 | 5.36 | |
| Sub Total | 52.3 | 61.62 | 3.58 | 2.52 | 0.137 | 0.008 | 0.067 | 0.066 | 5.40 | |
| Indicated | 4.4 | 60.01 | 4.76 | 2.50 | 0.065 | 0.025 | 0.037 | 0.101 | 6.39 | |
| Marra Mamba | I Inferred | 6.2 | 59.87 | 4.66 | 2.43 | 0.066 | 0.018 | 0.037 | 0.201 | 6.74 |
| Sub Total | 10.6 | 59.93 | 4.70 | 2.45 | 0.066 | 0.021 | 0.037 | 0.160 | 6.59 | |
| TOTAL | 62.9 | 61.33 | 3.77 | 2.51 | 0.125 | 0.010 | 0.062 | 0.082 | 5.60 |
The Brockman type ore of the Dales Gorge Member has high levels of phosphorus, whereas the Marra Mamba ore is low in phosphorus at 0.066% and can be utilised as a blend to the Brockman ore.
Tony Poli Executive Chairman
For further information regarding this announcement, please contact Tony Poli.
| Telephone: | $(08)$ 9423 0111 |
|---|---|
| Facsimile: | $(08)$ 9423 0133 |
| Email address: | [email protected] |
| Visit us at: | www.aquilaresources.com.au |
The information in this announcement that relates to Mineral Resources is based on information compiled by Mr Stuart H Tuckey, Dr Sia Khosrowshahi
and Mr Jani Kalla who are members of the Australian Institute of Mining and Tuckey. Dr Khosrowshahi and Mr Kalla consent to the inclusion in the report of the matters based on their information in the form and context in which it appears.
