中文摘要：

宏远（铜）钼矿和吐克吐克钼铜矿为新疆西准噶尔地区新发现的斑岩型矿床。流体包裹体测温和激光拉曼探针分析研究表明，宏远（铜）钼矿发育气液、气体和含子矿物包裹体等3类包裹体，气液比变化大，均一温度集中在140℃～200℃和260℃～340℃两个区间；吐克吐克钼铜矿只含有气液和含子矿物两类包裹体，气液比变化小，均一温度集中在180℃～220℃。两个矿区均发育高盐度和低盐度的NaCl-H20-CH4-CO2流体，显示含甲烷还原性流体的性质。宏远（铜）钼矿辉钼矿Re-0s同位素分析表明其成矿年龄为314．3±1．9Ma，与西准噶尔包古图斑岩铜矿成矿时代一致。

英文摘要：

Hongyuan（Cu） Mo deposit and Tuketuke Mo-Cu deposit are newly discovered porphyry- type deposits in the West Junggar region, Xinjiang. Microthermometry and Laser Raman Microprobe Analysis （LRM）of fluid inclusions indicate that there are three types of fluid inclusions at Hongyuan（Cu） Mo deposit,including aqueous fluid inclusions, gas inclusions and multi-phase fluid inclusions with daughter minerals. The gas-liquid ratios of fluid inclusions at Hongyuan（Cu） Mo deposit vary greatly. And homogenization temperatures concentrate in 140 % to 200 ℃ and 260 ℃ to 340 ℃. There are only two types of fluid inclusions at Tuketuke Mo-Cu deposit, aqueous fluid inclusions and multi-phase fluid inclusions with daughter minerals, with small changes of gas-liquid ratios. The homogenization temperatures at Tuketuke deposit concentrate in 180 ℃ to 220 ~℃. The two deposits both develop high-salinity and low-salinity NaC1-HEO-CH4-CO2 fluid system. And they both contain CH4, a kind of reductive fluid. The Re-Os isotope analysis of molybdenite from Hongyuan （Cu） Mo deposit indicates a mineralization age of 314.3± 1.9 Ma, consistent with Baogutu porphyry deposit in the West Junggar.