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    The Geology of Diamondoids (from mantle to brine component, lower to mid-crust)
    September 25, 2020
    Mud Volcanism and Seeps – (Black Shales)
    September 25, 2020
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    The Geology of Mud Volcanism

    By: Magma Chem Research Institute

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    Dolomitization, Silicification, Argillization and Late Carbonates – Calcite in UDH context (Sucrosic and saddle dolomite, silica and quarts, clays and black shales)

    The crystallization of other oxygen-rich minerals, such as dolomite, quartz, clay, and calcite, also contribute to the process of hydrogenation of kerogen by grabbing the oxygen from water, leaving the hydrogen free to attach to the kerogen. Sucrosic (sugary) dolomites are among the first to crystallize, followed by silica (quartz), clay (illite) in black shales, saddle dolomites, and finally calcite.

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    Dolomitization, Silicification, Argillization and Late Carbonates – Calcite in UDH context (Sucrosic and saddle dolomite, silica and quarts, clays and black shales)

    The crystallization of other oxygen-rich minerals, such as dolomite, quartz, clay, and calcite, also contribute to the process of hydrogenation of kerogen by grabbing the oxygen from water, leaving the hydrogen free to attach to the kerogen. Sucrosic (sugary) dolomites are among the first to crystallize, followed by silica (quartz), clay (illite) in black shales, saddle dolomites, and finally calcite.

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    Dolomitization, Silicification, Argillization and Late Carbonates – Calcite in UDH context (Sucrosic and saddle dolomite, silica and quarts, clays and black shales)

    The crystallization of other oxygen-rich minerals, such as dolomite, quartz, clay, and calcite, also contribute to the process of hydrogenation of kerogen by grabbing the oxygen from water, leaving the hydrogen free to attach to the kerogen. Sucrosic (sugary) dolomites are among the first to crystallize, followed by silica (quartz), clay (illite) in black shales, saddle dolomites, and finally calcite.

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