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Sericitic alteration or sericitization is a type of hydrothermal alteration characterized by the development of fine-grained white mica assemblages collectively referred to as sericite. In the Buchans–Roberts Arm Belt of Newfoundland, these assemblages include muscovitic illite, phengite, and paragonite associated with hydrothermal alteration zones.
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alteration hydrothermal assemblages sericite newfoundland muscovitic illite phengite paragonite sericitic sericitization type characterized development fine-grained white mica collectively referred buchans
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