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MINERALOGICAL FEATURES OF ULTRAMAFICHYPOXENOLITHS IN ALKALI-RICH PORPHYRY
作者姓名:LIUXianfan  YANGZhengxi  LIUJiaduo  ZHANGChengjiang  WUDechao  LIYouguo
作者单位:InstituteofEarthScience,ChengduUniversityofTechnology,ErxianqiaoDongsanRoad1#,Chengdu,SC610059,China
摘    要:Ultramafic hypoxenoliths found in the alkali-rich porphyry in the Liuhe Village, Heqing, Yunnan, China, are of great significance in understanding the origin and evolution of the porphyry. This paper discusses the mineralogical features of the hypoxenoliths. It shows that the xenoliths are characterized by the upper mantle rocks modified to certain extent by the enriched mantle fluid metasomatism in the mantle environment, with the enriched mantle property of low-degree partial melting. This constitutes the important mineralogical evidence for the petrogenesis and mineralization of alkali-rich porphyry. Keywords: alkali-rich porphyry; deep-source xenoliths; enriched mantle; low-degree partial melting; mineralogical characteristics

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MINERALOGICAL FEATURES OF ULTRAMAFIC HYPOXENOLITHS IN ALKALI-RICH PORPHYRY
LIUXianfan YANGZhengxi LIUJiaduo ZHANGChengjiang WUDechao LIYouguo.MINERALOGICAL FEATURES OF ULTRAMAFICHYPOXENOLITHS IN ALKALI-RICH PORPHYRY[J].Geotectonicaet Metallogenia,2003,27(1):81-90.
Authors:LIU Xianfan  YANG Zhengxi  LIU Jiaduo  Zhang Chengjiang  WU Dechao  Li Youguo
Abstract:Ultramafic hypoxenoliths found in the alkali-rich porphyry in the Liuhe Village, Heqing, Yunnan,China, are of great significance in understanding the origin and evolution of the porphyry. This paper discusses the mineralogical features of the hypoxenoliths. It shows that the xenoliths are characterized by the upper mantle rocks modified to certain extent by the enriched mantle fluid metasomatism in the mantle environment, with the enriched mantle property of Iow-degree partial melting. This constitutes the important mineralogical evidence for the petrogenesis and mineralization of alkali-rich porphyry.
Keywords:alkali-rich porphyry  deep-source xenoliths  enriched mantle  low-degree partial melting  mineralogical characteristics
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