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  2. Hydrothermal mineral deposit - Wikipedia

    en.wikipedia.org/wiki/Hydrothermal_mineral_deposit

    Hydrothermal mineral deposits are accumulations of valuable minerals which formed from hot waters circulating in Earth's crust through fractures. They eventually produce metallic -rich fluids concentrated in a selected volume of rock, which become supersaturated and then precipitate ore minerals.

  3. Category:Ore deposits - Wikipedia

    en.wikipedia.org/wiki/Category:Ore_deposits

    Download QR code; Print/export Download as PDF; Printable version; In other projects ... Heavy mineral sands ore deposits; Hydrothermal mineral deposit; I.

  4. Hydrothermal circulation - Wikipedia

    en.wikipedia.org/wiki/Hydrothermal_circulation

    Hydrothermal circulation in the oceans is the passage of the water through mid-oceanic ridge systems.. The term includes both the circulation of the well-known, high-temperature vent waters near the ridge crests, and the much-lower-temperature, diffuse flow of water through sediments and buried basalts further from the ridge crests. [3]

  5. Orogenic gold deposit - Wikipedia

    en.wikipedia.org/wiki/Orogenic_gold_deposit

    The Oubasi orogenic gold deposit in Southern Ghana is host to mineral resources of over 70 Moz Au at a grade of 7.39g/t or higher, with a past production of 32 Moz Au. [9] The deposit is located in the Birimian orogen, where gold mining is known to have taken place back to the 17th century, but modern industrial-scale mining began in 1897 by ...

  6. Ore genesis - Wikipedia

    en.wikipedia.org/wiki/Ore_genesis

    Epithermal — mineral ore deposits formed at low temperatures (50–200 °C) near the Earth's surface (<1500 m), that fill veins, breccias, and stockworks. [2] Telethermal — mineral ore deposits formed at shallow depth and relatively low temperatures, with little or no wall-rock alteration, presumably far from the source of hydrothermal ...

  7. Sedimentary exhalative deposits - Wikipedia

    en.wikipedia.org/.../Sedimentary_exhalative_deposits

    SEDEX deposits belong to the large class of non-magmatic hydrothermal ore deposits formed by basinal brines. [11] This class includes also: Mississippi valley type (MVT) zinc-lead deposits. [8] Sediment-hosted stratiform Cu-Co-(Ag) deposit, typified by the Copperbelt of Zambia and DRC. [12]

  8. Carlin–type gold deposit - Wikipedia

    en.wikipedia.org/wiki/Carlin–type_gold_deposit

    The Carlin–type deposits represent some of the largest hydrothermal gold deposits in the world. [7] The invisible nature of the gold in the deposit makes it difficult to find deposits of that kind. The class of deposit was defined after the Carlin mine became a mass producer of gold in the 1960s and it was recognized that other deposits of ...

  9. Deep water cycle - Wikipedia

    en.wikipedia.org/wiki/Deep_water_cycle

    Water content in magma determines how explosive a volcanic eruption is; hot water is the main conduit for economically important minerals to concentrate in hydrothermal mineral deposits; and water plays an important role in the formation and migration of petroleum. [3] Schematic of tectonic plate boundaries.