Difference between revisions of "Ternary and higher gem-like compounds"

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(The spinell group (wikipedia))
(The spinell group (wikipedia))
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* ZnAl<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Gahnite gahnite]
 
* ZnAl<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Gahnite gahnite]
 
* BeAl<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Chrysoberyl crysoberyll]
 
* BeAl<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Chrysoberyl crysoberyll]
* MnAl<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Galaxite galaxite] - (with rather rare manganese)
+
* MnAl<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Galaxite galaxite] - (with rather rare manganese) - [http://rruff.info/Spinel/R070013 image]
  
 
'''iron spinells'''
 
'''iron spinells'''
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* MgFe<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Magnesioferrite magnesioferrite]
 
* MgFe<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Magnesioferrite magnesioferrite]
 
* TiFe<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Ulv%C3%B6spinel ulvöspinel]   
 
* TiFe<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Ulv%C3%B6spinel ulvöspinel]   
* ZnFe<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Franklinite franklinite]    
+
* ZnFe<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Franklinite franklinite]
 +
* NiFe<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Trevorite trevorite]
 +
* MnFe<sub>2</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Jacobsite jacobsite] - (with rather rare manganese)
 
related compound:
 
related compound:
 
* ZnFe<sub>3</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Zinc_ferrite zinc ferrite] - synthetic zinc ferrites
 
* ZnFe<sub>3</sub>O<sub>4</sub> - wikipedia: [http://en.wikipedia.org/wiki/Zinc_ferrite zinc ferrite] - synthetic zinc ferrites

Revision as of 07:58, 14 February 2015

Look out for rock forming minerals here


Alkali and earth alkali compounds tend to be rather soluble in binary compounds (you won't find many there) in ternary and higher compounds they tend to form less water soluble minerals. See: compounds with s-block metals

most common metal rich core mantle transition zone minerals

In the earths mantle and crust silicon and oxygen are the most abundant elements. On the borther to earths outer core this changes to iron and nickle. Down there the most abundant minearls are made from mixture of those elements: olivine/peridot Of interest as diamondoid materials may be the pure end members of the mixing series:

In nature when iron rich metal is available in stochiometric excess heterogenous pallasite is formed. This rock looks really beautiful and can be found in some meteroids.

Another interesting tertiary material would be CSiO 4
a solid intermediate material between CO2(gas) SiO2(solid quartz): [1]

The spinell group (wikipedia)

These oxide minerals are devoid of the ubiquitously present silicon.

aluminum spinells

iron spinells

related compound:

  • ZnFe3O4 - wikipedia: zinc ferrite - synthetic zinc ferrites