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首页> 外文期刊>Mineralogy and Petrology >Ba-REE fluorcarbonate minerals from a carbonatite dyke at Bayan Obo, Inner Mongolia, North China
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Ba-REE fluorcarbonate minerals from a carbonatite dyke at Bayan Obo, Inner Mongolia, North China

机译:来自华北内蒙古巴彦鄂博的碳酸盐岩堤坝中的Ba-REE碳酸盐矿物

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摘要

The new occurrence in a carbonatite dyke at Bayan Obo, Inner Mongolia, North China, of the Ba-REE fluorocarbonate minerals cebaite, hunghoite and cordylite is presented, together with their chemical composition, rare earth element (REE) patterns, and syntaxial inter growth relationships. These syntaxial textures, investigated by scanning and electron microprobe techniques, are interpreted in terms of the cooling history during the late-stage crystallization of the carbonatite magma or possible later events. The REE distribution patterns of the Ba-REE fluorocarbonate minerals in the dyke are similar to those of the corresponding minerals in the dolomite marble that hosts the giant REE-Nb-Fe ore body at Bayan Obo, providing evidence that the two may be cogenetic.
机译:介绍了在华北内蒙古巴彦奥博的碳酸盐岩堤中新出现的Ba-REE氟碳酸盐矿物宿本石,红矾石和堇青石,以及它们的化学组成,稀土元素(REE)模式和句法互生关系。通过扫描和电子微探针技术研究的这些语法纹理,是根据碳酸盐岩浆后期结晶或可能发生的后续事件中的冷却历史来解释的。堤坝中的Ba-REE碳氟酸盐矿物的REE分布模式与在Bayan Obo拥有巨大的REE-Nb-Fe矿体的白云石大理石中的相应矿物相似,这提供了两者可能是共生的证据。

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