陕西凤太矿集区柴蚂金矿床成矿时代的^(40)Ar-^(39)Ar年龄证据  

Evidence of ^(40)Ar/^(39)Ar age data for ore-forming time of Chaima gold deposit in Fengtai ore concentration area,Shaanxi Province

作　　者：刘协鲁 王义天[2] 胡乔青[2] 王瑞廷 彭洛宏 张革利 刘敏[2] 欧阳升[5] LIU XieLu;WANG YiTian;HU QiaoQing;WANG RuiTing;PENG LuoHong;ZHANG GeLi;LIU Min;OUYANG She(Beijing Institute of Exploration Engineering, Beijing 100083, China;MLR Key Laboratory of Metallogeny and Mineral Assess- ment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;Geological Exploration In- stitute of Northwest Mining and Geology Group Co., Ltd., for Nonferrous Metals, Xi＇ an 710054, Shaanxi, China;Baoji No. 717 Brigade Company Ltd. of Northwest Nonferrous Metals, Baoji 721004, Shaanxi, China;Tongguan Bureau of Land and Resources, Tongguan 714300, Shaanxi, China)

机构地区：[1]北京探矿工程研究所,北京100083 [2]中国地质科学院矿产资源研究所国土资源部成矿作用和资源评价重点实验室,北京100037 [3]西北有色地质矿业集团有限公司地质勘查院,陕西西安710054 [4]宝鸡西北有色七一七总队有限公司,陕西宝鸡721004 [5]陕西省潼关县国土资源局,陕西潼关714300

出　　处：《矿床地质》2018年第1期163-174,共12页Mineral Deposits

基　　金：国家自然科学基金项目(编号:41372089);中国地质调查局地质调查工作项目(编号:1212011220869);中央级公益性科研院所基本科研业务费专项资金项目(编号:K0801)联合资助

摘　　要：柴蚂金矿床位于陕西凤太矿集区的西北部,矿体产于长沟-八卦庙向斜和长沟-打柴沟背斜核部和两翼的NWW向脆韧性剪切构造带中,赋矿地层为上泥盆统星红铺组的斑点状铁白云质粉砂质千枚岩。金矿化类型包括石英脉型和蚀变岩型2种。成矿过程划分为早期石英-碳酸盐阶段、主成矿期石英-碳酸盐-硫化物阶段和晚期石英脉阶段。对主成矿阶段热液蚀变形成的绢云母开展40Ar/39Ar测年研究,获得坪年龄为(219.0±2.0)Ma,指示其成矿作用始于219 Ma左右,即晚三叠世。前期工作获得该阶段碳酸盐矿物的Sm-Nd同位素年龄为(203.0±1.6)Ma,2个年龄值可能限定了成矿作用的上限与下限。结合前人有关区域地质与成矿作用的研究成果分析认为,柴蚂金矿床属于造山型金矿床,其成矿作用的多阶段性与剪切带长期演化过程中的构造递进变形密不可分。The Chaima gold deposit is located in the northwest of the Fengxian-Taibai （Fengtai） ore concentration area in Shaanxi Province. It is developed within a NWW-trending brittle-ductile shear zone. The orebodies are hosted in spotted ankerite-silty phyllite of Upper Devonian Xinghongpu Formation and occur in the limbs and cores of the Changgou-Baguamiao syncline and Changgou-Dachaigou anticline. The ores are mainly altered rock type and quartz-vein type. The gold mineralization could be divided into three stages：the early quartz-carbonate stage, the main quartz-carbonate-sulfide stage and the late quartz stage. In this paper, the ^40Ar-^39Ar dating was carried out on the sericite resulting from hydrothermal alteration in the main mineralization stage, yielding a plateau age of （219.0±2.0） Ma, which shows that the mineralization of the Chaima gold deposit started from 219 Ma. Combined with the carbonate minerals Sm-Nd isotopic age of （203.0±1.6） Ma obtained before, the age data may define the upper and lower limits of gold mineralization. Combined with previous work on the regional geology and polymetallic mineralization, the authors hold that the Chaima gold deposit is an orogenic gold deposit, whose multiple stages of mineralization were inseparable with the progressive deformation of the shear zone during the long-term tectonic evolution in Triassic.

关 键 词：地球化学 热液蚀变 绢云母 氩-氩测年 柴蚂金矿床 风太矿集区 

分 类 号：P618.31[天文地球—矿床学]