Teaching Mineralogy with Crystal Structure Databases and Visualization Software
Integrating Research and Education > Crystallography > Identifying Minerals Using Chemical and Crystallographic Data > Directions for CrystalMaker Users > Unknown #8

Unknown #8

Download and view the crystal structure data

  1. Right click on Unknown_8.cmdf ( 12kB Dec16 09) to download the crystal structure to your computer. (This file was modified from a CIF file in the Crystal Structure Library provided in CrystalMaker).
  2. Start the CrystalMaker program.
  3. Choose the File > Open command, and select the file you just downloaded to view in CrystalMaker.
  4. Click on OK to generate the crystal structure for viewing. You should see something like this...

Determine the identity of the unknown

Using your knowledge of crystallography and systematic mineralogy, and manipulating the downloaded structure in CrystalMaker, answer the following questions to deduce the identity of the unknown. Check your answers by clicking on the "show answer" tabs which appear with each question.
Click on Edit > Bonding to draw the Si-O bonds. Click on Add and choose "Si" under From and "O" under To. Follow the same procedure for adding the Al-O bonds. Clicking on the box under Info will give you information about coordination. Finally, click on OK to draw the bonds. The window should look like this...

Are the silica tetrahedra isolated or connected in some way? If connected, how? (hint: to highlight the tetrahedra, use the Model > Polyhedral command to plot the structure as a polyhedral model).
The silica tetrahedra are linked in a 3-dimensional network, making this mineral a tectosilicate.
showShow question #2
What crystal system does this mineral belong to?
showShow answer
Triclinic
showShow question #3
Why isn't the symmetry monoclinic?
showShow answer
Because of ordering of Si and Al tetrahedra in the structure.
showShow question #4
What is the other cation in this mineral besides Si and Al?
showShow answer
Calcium

...so what mineral is this?
Anorthite - CaAl2Si2O8
Anorthite

The structure is from Wainwright & Starkey (1971) Z Kristallogr 133:75-84.

The amount of Al in the tetrahedral site in this mineral is enough to make it a feldspar, but not enough to make it a feldspathoid. The presence of Ca as the sole non-tetrahedral cation indicates that it is Anorthite.

« Previous Page      Next Page »