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  2. Inclusion (mineral) - Wikipedia

    en.wikipedia.org/wiki/Inclusion_(mineral)

    In mineralogy, an inclusion is any material trapped inside a mineral during its formation. In gemology , it is an object enclosed within a gemstone or reaching its surface from the interior. [ 1 ] According to James Hutton 's law of inclusions, fragments included in a host rock are older than the host rock itself.

  3. Diamond inclusions - Wikipedia

    en.wikipedia.org/wiki/Diamond_inclusions

    The timing of mineral crystallization can be used to categorize diamond inclusions into three types: protogenetic, syngenetic, and epigenetic inclusions. [14] Minerals in the protogenetic inclusions were crystallized earlier than the diamond formation. The host diamond encapsulated pre-existing minerals during its crystallization.

  4. Fluid inclusion - Wikipedia

    en.wikipedia.org/wiki/Fluid_inclusion

    Hydrothermal ore minerals, which typically form from high temperature aqueous solutions, trap tiny bubbles of liquids or gases when cooling and forming solid rock. The trapped fluid in an inclusion preserves a record of the composition, temperature and pressure of the mineralizing environment. [1] An inclusion often contains two or more phases ...

  5. Portal:Minerals - Wikipedia

    en.wikipedia.org/wiki/Portal:Minerals

    The mineral is typically colorless or white, but may also be light blue, dark blue, purple, pink, red, orange, yellow or gray depending on inclusion of other materials, impurities, and structural or isotopic abnormalities in the crystals.

  6. Melt inclusion - Wikipedia

    en.wikipedia.org/wiki/Melt_inclusion

    Melt inclusions are generally small - most are less than 80 micrometres across (a micrometre is one thousandth of a millimeter, or about 0.00004 inches). [4] They may contain a number of different constituents, including glass (which represents melt that has been quenched by rapid cooling), small crystals and a separate vapour-rich bubble. [5]

  7. Siilinjärvi carbonatite - Wikipedia

    en.wikipedia.org/wiki/Siilinjärvi_carbonatite

    However, the grain size varies quite a lot, and large crystals with diameter of several centimeters are not uncommon. The largest found crystal clusters are up to 30 cm long. Inclusions are rare and the inclusion minerals are most commonly phlogopite and opaques. Altering of the mineral is uncommon. [52]

  8. Breyite - Wikipedia

    en.wikipedia.org/wiki/Breyite

    Breyite is a high pressure calcium silicate mineral (CaSiO 3) found in diamond inclusions. [3] [4] It is the second most abundant inclusion after ferropericlase, for diamonds with a deep Earth origin. [5] [4] Its occurrence can also indicate the host diamond's super-deep origin. This mineral is named after German mineralogist, petrologist and ...

  9. List of minerals - Wikipedia

    en.wikipedia.org/wiki/List_of_minerals

    This is a list of minerals which have Wikipedia articles. Minerals are distinguished by various chemical and physical properties. Differences in chemical composition and crystal structure distinguish the various species. Within a mineral species there may be variation in physical properties or minor amounts of impurities that are recognized by ...