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The fergusonite alkaline granite referred to in this paper is a complex consisting of acmite-augite riebeckite granite, riebeckite granite and biotite riebeckite granite. Its principal rock-forming minerals include acmite-augite, riebeckite, quartz, perthite and biotite, with fergusonite, zircon, magnetite and galena as its accessary minerals. Astrophyllite and thorite are abundant in a late alkali granite dike. Petrochemically, it is rich in K, Na, Si, and such rare metals as Nb, Ta, Y, Yb, Zr and Hf, but depleted in Al and Ca. In comparison with that found in other types of granite, the fergusonite in the alkaline granite has higher ferromagnesian components, thorium, niobium, but lower rare earths and tantalum. 相似文献
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Tantalite,occurring as intergranular tabular crystals,was reported for the first time in the Suzhou granite.Electron microprobe analyses show that it is rich in W and Ti,with a Ta/(Ta Nb) ratio ranging from 0.5 to 0.73 and a Mn(Mn Fe) ratio between 0.20 and 0.40.It is structurally distinct from isomorphic tapiolite by a remarked Ag Raman peak at 880cm^-1.The associated zircon is striking by significant enrichment of Hf,with the HfO2 content amounting up to 35%-40%,The discovery of tantalite suggests that the Suzhou granite should be classified as a S-type granite instead of A-type as considered previously. 相似文献
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