吉林省蛟河市新安屯钨钼矿流体包裹体、氢氧同位素及成矿时代研究
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摘要
吉林省蛟河市新安屯钨钼矿位于小兴安岭-张广才岭成矿带内,矿体呈细脉浸染状产于似斑状花岗闪长岩内,严格受北东向压扭性断裂构造控制。本文系统阐述了新安屯钨钼矿的区域地质背景、成矿地质特征,重点开展了流体包裹体、氢氧同位素及成矿时代等方面研究。结果表明,矿床成矿期流体均一温度180～235℃,流体盐度(3. 23～13. 82) wt%Na Cleqv,密度0. 875～0. 975 g/cm3,成矿深度0. 05～1. 1km;成矿流体中δ18O为9. 0‰～9. 8‰,δD为-106. 2‰～-116. 3‰;采用LA-ICP-MS锆石U-Pb法获得含矿似斑状花岗闪长岩成岩年龄为195. 4±1. 2Ma;通过辉钼矿Re-Os同位素法获得成矿年龄为180. 5±3. 9Ma。综合分析认为,该矿床成矿物质来自壳源,矿床类型属于断裂构造控制的浅成中低温岩浆热液型,成矿时代为早侏罗世,属于太平洋板块俯冲作用下的活动大陆边缘构造环境下的产物。
The Xin'antun W-Mo deposit of Jiaohe City,Jilin Province is situated in the Xiaoxinganling-Zhangguangcailing metallogenic belt,where the ore body occurs in byporphyroid granodiorite with veinlet-disseminated shape,controlled by northeast-east trending compression-shear fault structure. This article elucidates the regional geologic background and metallogenic characteristics of this deposit,focusing on the study of fluid inclusions,H-O isotope and metallogenic epoch. Results show that the homogeneous temperature of fluids was 180 ～ 235℃,the salinity of fluids was( 3. 23 ～ 13. 82)wt% NaC leqv,fluid density was 0. 875 ～ 0. 975 g/cm3,metallogenic depth was 0. 05 ～ 1. 1 km,and δ18 O was 9. 0‰ ～ 9. 8‰ and δD is-106. 2‰ ～-116. 3‰ in ore-forming fluid. The LA-ICP-MS zircon U-Pb age of ore-bearing byporphyroid granodiorite is 195. 4 ± 1. 2 Ma. The Re-Os isotopic dating yields an isochron age of 180. 5 ± 3. 9 Ma. Comprehensive analysis suggests that the mineralization material was originated from the crust. The deposit is of a meso-epithermal magmatic type controlled by fault structure. It was formed in the Early Jurassic along an active continental margin under the subduction of the Paleo-Pacific Plate.
The Xin'antun W-Mo deposit of Jiaohe City,Jilin Province is situated in the Xiaoxinganling-Zhangguangcailing metallogenic belt,where the ore body occurs in byporphyroid granodiorite with veinlet-disseminated shape,controlled by northeast-east trending compression-shear fault structure. This article elucidates the regional geologic background and metallogenic characteristics of this deposit,focusing on the study of fluid inclusions,H-O isotope and metallogenic epoch. Results show that the homogeneous temperature of fluids was 180 ～ 235℃,the salinity of fluids was( 3. 23 ～ 13. 82)wt% NaC leqv,fluid density was 0. 875 ～ 0. 975 g/cm3,metallogenic depth was 0. 05 ～ 1. 1 km,and δ18 O was 9. 0‰ ～ 9. 8‰ and δD is-106. 2‰ ～-116. 3‰ in ore-forming fluid. The LA-ICP-MS zircon U-Pb age of ore-bearing byporphyroid granodiorite is 195. 4 ± 1. 2 Ma. The Re-Os isotopic dating yields an isochron age of 180. 5 ± 3. 9 Ma. Comprehensive analysis suggests that the mineralization material was originated from the crust. The deposit is of a meso-epithermal magmatic type controlled by fault structure. It was formed in the Early Jurassic along an active continental margin under the subduction of the Paleo-Pacific Plate.
引文
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