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  2. Serpentine subgroup - Wikipedia

    en.wikipedia.org/wiki/Serpentine_subgroup

    Serpentine subgroup (part of the kaolinite-serpentine group in the category of phyllosilicates) [1] are greenish, brownish, or spotted minerals commonly found in serpentinite. They are used as a source of magnesium and asbestos , and as decorative stone. [ 5 ]

  3. Serpentinite - Wikipedia

    en.wikipedia.org/wiki/Serpentinite

    Serpentine group minerals have a Mohs hardness of 2.5 to 3.5, so serpentinite is easily carved. [26] Grades of serpentinite higher in calcite , along with the verd antique ( breccia form of serpentinite), have historically been used as decorative stones for their marble-like qualities.

  4. Connemara marble - Wikipedia

    en.wikipedia.org/wiki/Connemara_marble

    The distinct green colour of the middle slab is a result of an abundance of serpentine minerals Connemara marble ornament, Museum Building, Trinity College Dublin. Connemara marble or "Irish green" is a rare variety of green marble from Connemara, Ireland. It is used as a decoration and building material.

  5. Marble - Wikipedia

    en.wikipedia.org/wiki/Marble

    Construction marble is a stone which is composed of calcite, dolomite or serpentine that is capable of taking a polish. [20] More generally in construction , specifically the dimension stone trade, the term marble is used for any crystalline calcitic rock (and some non-calcitic rocks) useful as building stone.

  6. Verd antique - Wikipedia

    en.wikipedia.org/wiki/Verd_antique

    Verd antique is very similar in colour to the national gemstone of Ireland, Connemara marble.Connemara marble differs from the verd antiques in that it is an actual marble, rather than a serpentinite breccia, despite also having a very high serpentine content.

  7. Serpentinization - Wikipedia

    en.wikipedia.org/wiki/Serpentinization

    The mixture of brucite and serpentine formed by Reaction 1b has the lowest silica activity in the serpentinite, so that the brucite phase is very important in understanding serpentinization. [14] However, the brucite is often blended in with the serpentine such that it is difficult to identify except with X-ray diffraction , and it is easily ...

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