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STUDY ON THE ORE-FORMING CONDITIONS AND GENESIS OF TULING AND SHIHU GOLD DEPOSIT IN THE TAIHANG MOUNTAIN REGION

Yang Dianfan Li Gaoshan Jia Keshi(Changchun University of Earth Science)Wang Xuechun Ju Gui Wang Jingshu(Sixth Department Corporation of First Metallurgy Geological exploration Corpration)  
Tuling and Shihu gold deposit in Lingshou county,Hebei province occurred in metamorphic unit of Archean Fuping group.The ore bodiies are spatially controlled by structural shatter zone. The fracture controlling ore body have characteristics of multiple stages and composite as well as long time activity. The magmatic rock is very abundant. The Mapeng magma body is I-type granite. Its gold abundance value is 0.0097 ppm.Sulfur, Carbon,Oxygen as well as lead isotopes indicate that ore-forming fluid were derived from the magma rock.The Co/Ni ratio of pyrite is 2.59; The Au/Ag ratio is less than 0.5; the ore-forming temperature is about 190-373℃; Cl is more than F-,and Na+ is more than K+ in composition of quartz inclusions. These indicates that gold was probably transported as[AuCl2]-, [AuCl4]-, or[Aus]-in hydrothermal solution.Tuling,Shihu gold deposit in the Taihang mountain region is of vein-type gold deposit of post-magmatic hydrothermal.
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