Geological Characteristics and Fluid Inclusion Studiesof the Baogutu Porphyry Copper Deposit in West Junggar of Xinjiangoft-com:office:office" />
The Baoguto porphyry copper deposit locates in south of the Darbut magmatic arc of the western Junggar. The north-east regional structure mainly composed by a series of major faults. The Baogutu intrusion is intermediate porphyry with several lithologies and lithofacies. Mineralization type is disseminated mineralization,veinlets and network mineralization. The ore-forming process can divided into three phases. Fluid inclusions data showed:homogenization temperatures from the first stage to the third stage gradually reduced, indicating that mineralization from early and late going through a cooling process.oft-com:office:office" />
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