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  2. 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.

  3. Zirconium - Wikipedia

    en.wikipedia.org/wiki/Zirconium

    90 Zr, 91 Zr, 92 Zr and 94 Zr are stable, although 94 Zr is predicted to undergo double beta decay (not observed experimentally) with a half-life of more than 1.10×10 17 years. 96 Zr has a half-life of 2.34×10 19 years, and is the longest-lived radioisotope of zirconium. Of these natural isotopes, 90 Zr is the most common, making up 51.45% of ...

  4. Mineral (nutrient) - Wikipedia

    en.wikipedia.org/wiki/Mineral_(nutrient)

    Some "minerals" are essential for life, but most are not. [1] [2] [3] Minerals are one of the four groups of essential nutrients; the others are vitamins, essential fatty acids, and essential amino acids. [4] The five major minerals in the human body are calcium, phosphorus, potassium, sodium, and magnesium. [2]

  5. Thorium - Wikipedia

    en.wikipedia.org/wiki/Thorium

    Thorium only occurs as a minor constituent of most minerals, and was for this reason previously thought to be rare. [90] [91] In fact, it is the 37th most abundant element in the Earth's crust with an abundance of 12 parts per million. [92]

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  7. Mineral - Wikipedia

    en.wikipedia.org/wiki/Mineral

    The largest grouping of minerals by far are the silicates; most rocks are composed of greater than 95% silicate minerals, and over 90% of the Earth's crust is composed of these minerals. [102] The two main constituents of silicates are silicon and oxygen, which are the two most abundant elements in the Earth's crust.

  8. Feldspar - Wikipedia

    en.wikipedia.org/wiki/Feldspar

    bytownite (70 to 90) (NaSi,CaAl)AlSi 2 O 8; anorthite (90 to 100) CaAl 2 Si 2 O 8; Intermediate compositions of exsolve to two feldspars of contrasting composition during cooling, but diffusion is much slower than in alkali feldspar, and the resulting two-feldspar intergrowths typically are too fine-grained to be visible with optical microscopes.

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