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Deep xenoliths in alkalic porphyry, Liuhe, Yunnan, and implications to petrogenesis of alkalic porphyry and associated mineralizations
Authors:Xianfan Liu  Xinzhi Zhan  Zhenmin Gao  Jiajun Liu  Chaoyang Li  Wenchao Su
Institution:(1) Open Laboratory of Geochemical Research, Institute of Geochemistry, Chinese Academy of Sciences, 550002 Guiyang, China;(2) Chengdu Institute of Technology, 610059 Chengdu, China
Abstract:Na-rich microlite-glass is first discovered in deep-source xenoliths in alkali-rich porphyry, Liuhe village, Heqing County, Yunnan Province. It is shown that the ultramafic xenoliths originated from partial melting of primary mantle and the glass resulted from metasomatism between the xenoliths and mantle fluid derived from mantle degassing. Mantle metasomatism not only resulted in the enrichment of alkaline, large-ion elements, ore metals and volatiles but also created a favorable condition for the generation of alkaline magmas. The mantle xenoliths and their characteristics of mantle metasomatism provide important evidence for a better understanding of the petrogenesis and mineralization of the Cenozoic alkali-rich porphyry in western Yunnan.
Keywords:deep xenoliths  mantle metasomatism  alkali-rich porphyry  petrogenesis and mineralization
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