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SERICITIC ALTERATION

  • Sericitic alteration
  • Process of mineral alteration

    Sericitic alteration or sericitization is a type of hydrothermal alteration characterized by the development of fine-grained white mica assemblages collectively

    Sericitic alteration

    Sericitic_alteration

  • Argillic alteration
  • tourmaline, enargite and tennantite may also occur. Greisen alteration is similar. Sericitic alteration Guilbert, John M. and C. F. Park, Jr., The Geology of

    Argillic alteration

    Argillic_alteration

  • Phyllic alteration
  • Geological process

    Plagioclase will be altered to sericite (a fine-grained white mica) by sericitic alteration, and mafic minerals are replaced by quartz. Tourmaline may appear

    Phyllic alteration

    Phyllic_alteration

  • Sericite
  • Aggregates of micas

    the alteration of orthoclase or plagioclase feldspars in areas that have been subjected to hydrothermal alteration (also see Sericitic alteration) typically

    Sericite

    Sericite

    Sericite

  • I-type granite
  • Subclass of granite formed from igneous protoliths

    atmosphere. Alteration of biotites can produce fluorite, chlorite, and iron oxides such as magnetite and ilmenite. Sericitic alteration is seen within

    I-type granite

    I-type_granite

  • Woodlark Basin
  • Oceanic basin located to the east of the island of New Guinea

    processes, silicification, chloritization, formation of illite, sericitic alteration, replacement of plagioclase by albite, and sulfidation associated

    Woodlark Basin

    Woodlark Basin

    Woodlark_Basin

  • Quartz-porphyry
  • Type of volcanic rock containing large porphyritic crystals of quartz

    this way they become schistose, and from their feldspar minute plates of sericitic white mica are developed, giving the rock in some cases very much of the

    Quartz-porphyry

    Quartz-porphyry

    Quartz-porphyry

  • Hajigak mining concession
  • Place in Maidan Wardak and Bamyan, Afghanistan

    500 m (14,800 ft) thick. The Kab Formation consists of dark grey sandy sericitic schists, interpreted as metamorphosed terrigenous rocks, acid volcanic

    Hajigak mining concession

    Hajigak_mining_concession

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