摘要
///The Jinshajiang-Ailaoshan faulting belt in western Yunnan Province were found to host the Cenozoic alkali-rich porphyries, of which the Liuhe syenite porphyry contains granite xenolith paragenetically associated with deep mafic and ultramafic xenoliths. CL imaging LA-ICP-MS U-Pb dating and trace element analysis for the zircon from granite xenoliths conducted were conducted in this study. The results show that the zircons in the xenoliths contain three types: 1) magmatic zircons, compound magmatic zircons with old cores and new growth zones, and metamorphic zircons; 2) the old core has an average weighted age of (828.1±7.1) Ma, which represents the age of basal rock; and 3) the metamorphic zircons have an average weighted 206Pb/238Pb age of (108.4±4.4) Ma, which is consistent with the age (102.87±1.19 Ma) of amphiboled flogopite garnet bistagite and represents the crystallization age of mantle fluid metasoatism.