|The Mineral Resource
Description of Operations
Diagram of Operations
Mine Closure Planning
The Mineral Resource
The Ok Tedi ore body lies within Mt Fubilan and contains copper, gold and silver mineralisation.
Gold production began at Ok Tedi in 1984 and the copper processing facilities were commissioned in 1987.
Due to the presence of a copper-leached residual gold cap over the main ore body, mining was planned in three phases:
Mining and processing of oxide gold ore from the gold cap.
Extraction and treatment of both sulphide copper and oxide gold ore.
Mining the main copper ore body, which includes porphyry and skarn ores. Both copper and gold are extracted from the ore body and sold as concentrates.
The major rock types in the region are continental margin marine sedimentary rocks (siltstones and limestones). Large-scale folds and thrust faults form the dominant structural features, with a large sheet of Darai Limestone thrust over siltstone in the mine area.
The fold belt is developed along the southern margin of a transition zone between two major geologic provinces: the Australian Plate to the south and the Pacific Plate to the north. The transition zone is also a region of rapid uplift and erosion dated from 2.6 to 0.7 million years.
The major rock types used for geologic modelling at the Ok Tedi mine are:
At 31 December 2004, the Ok Tedi mine had produced 8,896,577 tonnes of copper concentrate containing 2,853,265 tonnes of copper metal and 7,035,477 ounces of gold metal. Between 1985 and 1990 it also produced 1,680,553 ounces of gold bullion.
Ok Tedi's estimated proven and probable reserves as at 31 December 2004 were:
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Under 40 per cent of the Ok Tedi ore body remains to be mined between 2004 and mine closure in 2012.