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The geology, structure and mineralisation of the Oyu Tolgoi porphyry copper-gold-molybdenum deposits, Mongolia: A review
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文摘

The Oyu Tolgoi porphyry Cu-Au-Mo deposits lie within the Central Asian Orogenic Belt.

Ore occurs as telescoped prograde porphyry, phyllic retrograde and high sulphidation overprints.

High grade ore is controlled by a structural corridor, repeated intrusion and reactive host rocks.

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