熊小林, 朱金初, 饶冰
Abstract
Topaz was previously considered as a typical hydrothermal mineral, and topaz greisen a typically altered rock. However, the geological and geochemical evidence in recent years has made it clear that the layer-like topaz greisen at the top of Ta- and Nb-bearing albite
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Topaz was previously considered as a typical hydrothermal mineral, and topaz greisen a typically altered rock. However, the geological and geochemical evidence in recent years has made it clear that the layer-like topaz greisen at the top of Ta- and Nb-bearing albite
Key concepts: Topaz, Greisen, Albite, Geology, Cassiterite, Hydrothermal circulation, Geochemistry, Materials science