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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. 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 ...

  5. Herkimer diamond - Wikipedia

    en.wikipedia.org/wiki/Herkimer_diamond

    The geologic history of these crystals began about 500 million years ago in a shallow sea which was receiving sediments from the ancient Adirondack Mountains to the north. . The calcium and magnesium carbonate sediments accumulated and lithified to form the dolomite bedrock currently known as the Little Falls Formation and formerly as the Little Falls Dolostone.

  6. Mafic - Wikipedia

    en.wikipedia.org/wiki/Mafic

    A mafic mineral or rock is a silicate mineral or igneous rock rich in magnesium and iron. Most mafic minerals are dark in color, and common rock-forming mafic minerals include olivine, pyroxene, amphibole, and biotite. Common mafic rocks include basalt, diabase and gabbro. Mafic rocks often also contain calcium-rich varieties of plagioclase ...

  7. Peridot - Wikipedia

    en.wikipedia.org/wiki/Peridot

    The most common mineral inclusion in peridot is the chromium-rich mineral chromite. Magnesium-rich minerals also can exist in the form of pyrope and magnesiochromite. These two types of mineral inclusions are typically surrounded "lily-pad" cleavages. Biotite flakes appear flat, brown, translucent, and tabular. [16]

  8. Why Diversity Matters Catalyst 7-16-12 - HuffPost

    images.huffingtonpost.com/2013-03-21-why...

    Leaders working to create diverse and inclusive workplaces in which women can advance must make the connection between diversity initiatives and their organization’s business goals.1 Effective business cases set the context for diversity and identify organizational challenges that must be addressed in order to create change.

  9. Lamprophyre - Wikipedia

    en.wikipedia.org/wiki/Lamprophyre

    They are usually dark in color, owing to the abundance of ferro-magnesian silicates, of high specific gravity and liable to decomposition. For these reasons they have been defined as a melanocrate series (rich in the dark minerals ); and they are often accompanied by a complementary leucocrate series (rich in the white minerals feldspar and ...