No. Very common to have deviations from stiochiometric ratios in minerals.
Consider a form of limestone (Ca, Mg)CO3 where an indeterminent proportion of the Ca has been substituted by Mg.
Or intermetallic compounds. Suppose two metals A and B nominally form the intermetallic comppound A3B There may be some lattitude in that
ratio which causes the crystal matrix to become strained but still stable. Hence A2.96-3.04B[/rquot
Interesting! Can you supply a reference to this subject? I guess I confuse minerals with rocks. Thanks |