Airí a léiríonn criostail áirithe ina mbíonn luas forleata an tsolais difriúil i dtreonna difriúla mar thoradh ar a struchtúr criostalta. Bíonn dhá chomhéifeacht athraonta shainiúla ag criostail dhé-athraonacha cosúil le cailcít is grianchloch, agus is féidir íomhánna dúbailte a dhéanamh leo.[1]
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