Anagram & Information om | Engelska ordet ZOISITE
ZOISITE
Antal bokstäver
7
Är palindrom
Nej
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Exempel på hur man kan använda ZOISITE i en mening
- Tanzanite is the blue and violet variety of the mineral zoisite (a calcium aluminium hydroxyl sorosilicate), caused by small amounts of vanadium.
- Anyolite is a metamorphic rock composed of intergrown green zoisite, black/dark green pargasite and ruby.
- Thulite (sometimes called rosaline) is a translucent, crystalline or massive pink manganese-bearing variety of the mineral zoisite.
- Clinozoisite is green, white or pale rose-red group species containing very little iron, thus having the same chemical composition as the orthorhombic mineral zoisite.
- The names of Queen Beryl and the Four Kings of Heaven are derived from minerals: beryl, jadeite, nephrite, zoisite, and kunzite.
- Accessory minerals include kyanite, rutile, quartz, lawsonite, coesite, amphibole, phengite, paragonite, zoisite, dolomite, corundum and, rarely, diamond.
- It occurs in association with magnetite, sphalerite, chalcopyrite, skutterudite, allanite, zoisite, scapolite, titanite, and calcite along with numerous other Co–Ni sulfides and arsenides.
- Saussurite is not however recognized as a true mineral because it is a microscopic mixture of several other minerals, zoisite, epidote, sericite, albite or other sodium-rich feldspar along with possibly scapolite.
- Glaucophane, garnet, phengite, and zoisite or other epidote-group minerals are other common minerals in blueschist.
- Approximately 90–95% of that water is contained in hydrous minerals, including mica, phengite, amphibole, lawsonite, chlorite, talc, zoisite, and serpentine.
- The grain composition of the lithic fraction comprises zircon, epidote, zoisite, clinozoisite and pyroxenes, which at the top of the formation amounts to 86 percent.
- It is notable for tourmaline-rich zones containing accessory fuchsite, purple muscovite, epidote, clinozoisite, zoisite, thulite, tremolite, sillimanite, kyanite, cyprine, allanite, and stibiotantalite.
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