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Serpentine Research Paper

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Serpentine in Staten Island early Paleozoic times are formed are formed in a geological low-temperature metamorphic process in which involving heat and water. This process involves heat and water also in which low-silica mafic and ultramafic rocks are oxidized as well as hydrolyzed with water into serpentine. Peridotite, including, dunite, at and near the seafloor and in mountain belts is also converted to Serpentine, as well as brucite, and magnetite other minerals, and even native iron.

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