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  2. Orogenic gold deposit - Wikipedia

    en.wikipedia.org/wiki/Orogenic_gold_deposit

    An orogenic gold deposit is a type of hydrothermal mineral deposit. ... In magmatic systems, ores and host rocks are derived from the same fluid. [11]

  3. Ore genesis - Wikipedia

    en.wikipedia.org/wiki/Ore_genesis

    High-grade gold ore from the Harvard Mine, Jamestown, California, a wide quartz-gold vein in California's Mother Lode.Specimen is 3.2 cm (1.3 in) wide. Various theories of ore genesis explain how the various types of mineral deposits form within Earth's crust.

  4. Hydrothermal mineral deposit - Wikipedia

    en.wikipedia.org/wiki/Hydrothermal_mineral_deposit

    Ascending hydrothermal solutions rich in gold, sulfur and metals were channelled upward along major fracture and fault zones. Fluid that made it to the surface would have vented as hot springs and geysers. Localized erosion through the thrust sheet has formed windows into the underlying ore-bearing rocks. Adapted from Edwards and Atkinson (1985).

  5. Reko Diq Mine - Wikipedia

    en.wikipedia.org/wiki/Reko_Diq_Mine

    The Reko Diq Mine is a planned mining operation, located near Reko Diq town in Chagai District, Baluchistan, Pakistan. [1] Reko Diq represents one of the largest copper and gold reserves in the world having estimated reserves of 5.9 billion tonnes of ore grading 0.41% copper and gold reserves amounting to 41.5 million oz, and a mining life of at least 40 years.

  6. Iron oxide copper gold ore deposits - Wikipedia

    en.wikipedia.org/wiki/Iron_oxide_copper_gold_ore...

    Iron oxide copper gold (IOCG) deposits are considered to be metasomatic expressions of large crustal-scale alteration events driven by intrusive activity. The deposit type was first recognised by discovery and study of the supergiant Olympic Dam copper-gold-uranium deposit (Olympic Dam mine), and South American examples.

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  8. Igneous differentiation - Wikipedia

    en.wikipedia.org/wiki/Igneous_differentiation

    In geology, igneous differentiation, or magmatic differentiation, is an umbrella term for the various processes by which magmas undergo bulk chemical change during the partial melting process, cooling, emplacement, or eruption. The sequence of (usually increasingly silicic) magmas produced by igneous differentiation is known as a magma series.

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