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近几年来,对位于蒂尔内阿乌兹矿田内的前缘山脊带东缘发育的超基性岩所进行的研究,说明了与原始结晶作用有关的这些岩石是岩浆成因的,其成分很可能近于纯橄榄岩。
In recent years, the study on the ultramafic rocks developed on the eastern edge of the ridge of ridge in the Tierneauz field shows that these rocks related to the original crystallization are of magmatic origin, and their composition is very Probably near dunite.