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olivine

American  
[ol-uh-veen, ol-uh-veen] / ˈɒl əˌvin, ˌɒl əˈvin /

noun

  1. Mineralogy. any of a group of magnesium iron silicates, (Mg,Fe) 2 SiO 4 , occurring in olive-green to gray-green masses as an important constituent of basic igneous rocks.


olivine British  
/ ˌɒlɪˈviːn, ˈɒlɪˌviːn /

noun

  1. Also called: chrysolite.  an olive-green mineral of the olivine group, found in igneous and metamorphic rocks. The clear-green variety (peridot) is used as a gemstone. Composition: magnesium iron silicate. Formula: (MgFe) 2 SiO 4 . Crystal structure: orthorhombic

  2. any mineral in the group having the general formula (Mg,Fe,Mn,Ca) 2 SiO 4

"Collins English Dictionary — Complete & Unabridged" 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

olivine Scientific  
/ ŏlə-vēn′ /
  1. An olive-green to brownish-green orthorhombic mineral. Olivine is a common mineral in the igneous rocks, such as basalt and gabbro, that make up most of the Earth's crust beneath the oceans. Chemical formula: (Mg,Fe) 2 SiO 4 .

  2. ◆ Olivine in which the mafic component consists entirely of magnesium is called forsterite. Chemical formula: Mg 2 SiO 4 .

  3. ◆ Olivine in which the mafic component consists entirely of iron is called fayalite. Chemical formula: Fe 2 SiO 4 .


Other Word Forms

  • olivinic adjective
  • olivinitic adjective

Etymology

Origin of olivine

1785–95; < German Olivin, equivalent to Olive olive + -in -ine 2

Example Sentences

Examples are provided to illustrate real-world usage of words in context. Any opinions expressed do not reflect the views of Dictionary.com.

However, the team identifies a different class of relatively pristine asteroids that display olivine and spinel signatures as more promising mining targets.

From Science Daily

The Grenoble group analyzed strontium isotopes and trace elements in melt inclusions trapped inside 3.3-billion-year-old olivine crystals, providing rare geochemical snapshots of early Earth.

From Science Daily

On Earth, basalts are a main component of the planet's crust, especially under the oceans, while olivines are abundant in its mantle.

From Science Daily

They are produced in a number of ways but the main process involves the interaction of ground water with iron-rich minerals such as olivine.

From BBC

Alkaline materials such as limestone or olivine could be ground up or dissolved in water and then poured into the ocean from a ship.

From Science Magazine