What is seen the interference colour?

 

The interference colour is observed under the petrographic microscope with the analyser incorporated (in crossed-polarised light, XPL) and with parallel light (without the condenser).

rock       soil

Sometimes the minerals have an abnormal color that does not correspond to their birefringence.

A typical example of an abnormal interference color is chlorite.
XPL.Chlorite abnormal interference color: Blue PPL. Chlorite natural color: green

 

Most often, the abnormal interference color is due to the mineral's own natural color. This occurs whenever the mineral has an intense natural color.

A typical example is biotite.

     

Also other minerals present anomalous interference colors.

       
       
       
       
       

 

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