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《Journal of Jilin University(Earth Science Edition)》 2010-02
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Geological & Geochemical Characteristics and Metallogenesis of Sanjiazi Scheelite Deposit in Siping Area,Jilin Province

REN Yun-sheng1,NIU Jun-ping1,2,LEI En1,WANG Hui1,WANG Xi11.College of Earth Sciences,Jilin University,Changchun 130061,China2.Geophysical Exploration Institute of Jilin Province,Changchun 130012,China  
Sanjiazi deposit is one of the scheelite deposits in Northeastern China found in recent years.In order to discuss the metallogenesis,their geological and geochemical characteristics of the deposit is studied,including the composition of REE and trace elements in metallogenic granitic rocks,marble wall rock as well as in skarn ores.These granitic rocks containing scheelite mineralization,has similar geochemical features with those of the I-type granites, such as aluminium super-saturation,variable alkaline composition,K_2ONa_2O and low ratio of Rb/Sr.Moreover,the facts of low content of REE,negative δEu anomalies,unobvious δCe anomalies and right-declining chondrite-normalized REE patters demonstrate that tungsten-bearing granitic rocks was derived from deep crust or upper mantle.Together with geological features of the deposit,contents of trace elements and sulfur isotope in different rocks and ores,a conclusion can be drawn that the ore-forming materials,including W element,may come from the Mengjialing intrusion.The Sanjiazi scheelite deposit belongs to the skarn deposit and is related to the NW subduction of the Pacific plate underneath Eurasia plate in the Early Yanshanian period.
【Fund】: 中国科学院地球化学研究所矿床地球化学国家重点实验室开放基金项目(200904);; 高校“211”建设项目
【CateGory Index】: P618.67
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