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Geologic and geochemical features of the volatile-rich ore fluid and its tracing and dating in the Xuebaoding Beryl-Scheelite Vein Deposit,China 被引量:6
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作者 曹志敏 任建国 +6 位作者 郑建斌 徐仕进 李佑国 王汝成 T.SHOJ h.kaneda S.KABAYASHI 《Science China Earth Sciences》 SCIE EI CAS 2002年第8期719-729,共11页
Laser Raman spectrochemical analysis on single inclusion reveals that multi-phase fluid inclusions exist in the Xuebaoding Beryl- Scheelite Vein Deposit. Besides the solid daughter mineral, there are vapor CO2, liquid... Laser Raman spectrochemical analysis on single inclusion reveals that multi-phase fluid inclusions exist in the Xuebaoding Beryl- Scheelite Vein Deposit. Besides the solid daughter mineral, there are vapor CO2, liquid CO2, water-deficient CO2 and salt water solution from its center to the border. A close study on the fluid inclusion components and carbon, oxygen, helium and argon isotope tracing and dating suggests that the volatile-rich ore fluid might derive from postmagmatic fluid and rare element enrichment is the result of the mixture of the plutonic alkali granite with crustal material. 展开更多
关键词 multi-phase FLUID inclusion NOBLE gases isotope Beryl- SCHEELITE VEIN Deposit.
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