Overview
Stage | Production |
Mine Type | Open Pit |
Commodities |
|
Mining Method |
|
Processing |
- Gravity separation
- Crush & Screen plant
- Spiral concentrator / separator
- Dry Screening
- Desliming
|
Mine Life | 2024 |
The mine is operated by Rio Tinto as part of the Greater Paraburdoo mining hub. |
Source:
p. 384
Rio Tinto owns 54% of the Bao-Hi joint venture with the remaining 46% held by China Baowu
Summary:
Mineralisation at Eastern Range occurs as haematite/goethite mineralisation hosted within the banded iron formations of the Brockman Formation.
The Pilbara region comprises a large part of the ancient continental shield of Western Australia which is comprised of both Proterozoic and Archaean rocks. The Pilbara is overlain by the Proterozoics deposited in the Hamersley and Bangernall Provinces.
The BIF is a member of the ~620 m thick Brockman Iron Formation which makes up part of the 2.63 2.45 Ga Hamersley Group. The Hamersley Group comprises almost 2.5 km of consecutive sedimentary and volcanic rocks located within the ca. 80,000 km2 Hamersley Province of the Pilbara craton in North West Australia, approximately 1100 km north of Perth. In the lower part, it consists of dolomite, shale and BIF, while the upper part consists of dolerite, various lava types and BIF with minor amounts of tuffs and shales. Underlying the Hamersley Group, is the 2.78–2.63 Ga Fortescue Group, which consists of flood basalts and rhyolites. These volcanics were laid down on the uplifted and eroded Pilbara block. This volcanic succession may contain remnants of a Large Igneous Province (LIP).
The Brockman Iron Formation ofthe Hamersley Group is divided into four sub-lithostratigraphic units, namely the lowermost Dales Gorge Member (BIF), the Whaleback Shale Member, the Joffre Member (BIF), and the uppermost Yandicoogina Shale Member. After deposition, these laterally extensive BIF have all experienced minor folding and basinal uplift along with low-grade regional metamorphism – from burial prehnite–pumpellyite facies to greenschist facies.
General consensus exists regarding the depositional model of the Brockman Iron Formation. According to this model, the succession was deposited on a large, stable, and clastic-starved, continental platform, which was influenced by episodic inputs of fine-grained tuffaceous detritus.
Summary:
The Eastern Range iron ore mine is located in the Pilbara region of Western Australia, with the closest town being Paraburdoo, 8 km to the north. It falls within the local authority of the Shire of Ashburton. The mine is operated by Rio Tinto as part of the Greater Paraburdoo mining hub. Operations at Eastern Range span deposits at 23-24 East, 32 East, 37-42 East, 42 East and future mining at 42EE and the 47E deposits.
Ore is extracted using traditional open pit, drill and blast and load and haul methods.
Processing
- Gravity separation
- Crush & Screen plant
- Spiral concentrator / separator
- Dry Screening
- Desliming
Source:
Summary:
Ore from the Eastern Range mine is crushed and then processed through the central Paraburdoo tertiary crushing and dry screening plant to produce a dry lump product, with further wet processing of the fines product using hydrocyclones to remove slimes.
Reserves at December 31, 2020:
Category | Tonnage | Commodity | Grade |
Proven
|
18 Mt
|
Iron
|
61.4 %
|
Probable
|
4 Mt
|
Iron
|
60.3 %
|
Proven & Probable
|
22 Mt
|
Iron
|
61.2 %
|
Measured
|
22 Mt
|
Iron
|
60 %
|
Indicated
|
7 Mt
|
Iron
|
60 %
|
Inferred
|
2 Mt
|
Iron
|
59.2 %
|
Total Resource
|
31 Mt
|
Iron
|
60 %
|
Mine Management:
Job Title | Name | Profile | Ref. Date |
.......................
|
.......................
|
|
May 5, 2022
|
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Corporate Filings & Presentations:
Document | Year |
...................................
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2021
|
...................................
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2020
|
...................................
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2019
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Other
|
2016
|
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Aerial view:
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