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《Earth Science Frontiers》 2001-04
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CARBONATITIC FLUIDS AND REE MINERALIZATION

FAN Hong rui 1, XIE Yi han 1, WANG Kai yi 1,YANG Xue ming 2 (1.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029,China; 2.Department of Earth and Space Science, University of Science and Technology of China, Hefei  
Igneous carbonatites can intrude into both continental and oceanic tectonic settings. Most carbonatites in continental settings are associated in space and time with events of crustal thinning. The carbonated alkaline melt shows the high capability of transporting large ion lithophile and high field strength elements at high temperatures. Primary fluid inclusions in carbonatite complex generally comprise liquid vapour, daughter mineral bearing aqueous, CO 2 bearing, CO 2 + daughter mineral bearing solid, and silicate melting inclusions. Fluid inclusions in REE deposits can also be distinguished into liquid vapour, aqueous carbonic and aqueous liquid vapour solid inclusions. REE minerals identified as daughter inclusions are the special feature in this type of deposit. Alkali carbonatite fluids are capable of transporting huge amounts of REE, Sr, Th and Fe. The interaction of the fluids with carbonate host rocks and the fluid immiscibility are the key factors in the precipitation of both REE minerals and Fe oxides. The transport and precipitation of REE can last to the late stage of fluid influx despite of low temperatures and salinities.
【Fund】: 国家自然科学基金资助项目 ( 49972 0 36);; 中国科学院重 大资助项目 (KZCX1 0 7)
【CateGory Index】: P611
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