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  2. Zircon - Wikipedia

    en.wikipedia.org/wiki/Zircon

    Zircon ( / ˈzɜːrkɒn, - kən /) [ 7][ 8][ 9] is a mineral belonging to the group of nesosilicates and is a source of the metal zirconium. Its chemical name is zirconium (IV) silicate, and its corresponding chemical formula is Zr SiO 4. An empirical formula showing some of the range of substitution in zircon is (Zr 1–y, REE y ) (SiO 4) 1 ...

  3. Hadean zircon - Wikipedia

    en.wikipedia.org/wiki/Hadean_zircon

    Hadean zircon is the oldest-surviving crustal material from the Earth's earliest geological time period, the Hadean eon, about 4 billion years ago. Zircon is a mineral that is commonly used for radiometric dating because it is highly resistant to chemical changes and appears in the form of small crystals or grains in most igneous and metamorphic host rocks.

  4. File:MT RRocks zircon.pdf - Wikipedia

    en.wikipedia.org/wiki/File:MT_RRocks_zircon.pdf

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  5. Zirconium(IV) silicate - Wikipedia

    en.wikipedia.org/wiki/Zirconium(IV)_silicate

    Zirconium silicate, also zirconium orthosilicate, ZrSiO 4, is a chemical compound, a silicate of zirconium. It occurs in nature as zircon, a silicate mineral. Powdered zirconium silicate is also known as zircon flour. Zirconium silicate is usually colorless, but impurities induce various colorations. It is insoluble in water, acids, alkali and ...

  6. Zirconium dioxide - Wikipedia

    en.wikipedia.org/wiki/Zirconium_dioxide

    Zirconium dioxide ( ZrO. 2 ), sometimes known as zirconia (not to be confused with zircon ), is a white crystalline oxide of zirconium. Its most naturally occurring form, with a monoclinic crystalline structure, is the mineral baddeleyite. A dopant [clarification needed] stabilized cubic structured zirconia, cubic zirconia, is synthesized in ...

  7. Myrmekite - Wikipedia

    en.wikipedia.org/wiki/Myrmekite

    Myrmekite. Myrmekite is a vermicular, or wormy, intergrowth of quartz in plagioclase. The intergrowths are microscopic in scale, typically with maximum dimensions less than 1 millimeter. The plagioclase is sodium -rich, usually albite or oligoclase. These quartz-plagioclase intergrowths are associated with and commonly in contact with potassium ...

  8. ZTR index - Wikipedia

    en.wikipedia.org/wiki/ZTR_index

    ZTR index. The ZTR index is a method of determining how weathered, [1] both chemically and mechanically, a sediment (or a corresponding sedimentary rock) is. The letters in ZTR stand for 3 common minerals found in ultra-weathered sediments: zircon, tourmaline, and rutile. Other minerals that can be used alongside the ZTR index are garnet ...

  9. Zirconocene dichloride - Wikipedia

    en.wikipedia.org/wiki/Zirconocene_dichloride

    Zirconocene dichloride reacts with lithium aluminium hydride to give Cp 2 ZrHCl Schwartz's reagent: (C 5 H 5) 2 ZrCl 2 + 1 / 4 LiAlH 4 → (C 5 H 5) 2 ZrHCl + 1 / 4 LiAlCl 4. Since lithium aluminium hydride is a strong reductant, some over-reduction occurs to give the dihydrido complex, Cp 2 ZrH 2; treatment of the product mixture with methylene chloride converts it to Schwartz's reagent.