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《Contributions To Geology and Mineral Resources Research》 1989-01
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CHARACTERISTICS OF ZHI LINGTOU Au-Ag DEPOSIT IN ZHEJIANG PROVINCE

Xu Jinkun The Zhejiang Provincial geological Team  
This ore deposit and ore bodies occur as veins in a fractured zone (trending roughly E-W) developed in the metamorphosed rock of Chencai Group. The ore veins are arranged as en echelon. Ore-forming elements are dominated by gold and silver. There are two main mineralization i. e. sulfide-poor-gold (silver)-quartz veins and Au (Ag) -multi-metal quartz veins. Wall rock alterations of silicification sericitzation and Pyritization are symmetricaly developed. Zhi Lingtou area is located in a low grade metamorphism belt with well development of fractures and high Au-abundance. And here is the geothermal anomly area during Late Jurassic and Early Cretaceous. All this is the special condition favourably to form this deposit. The deposit were formed during Late Yanshan Movement as a super-hydrothermal Au-deposit whose ore-forming materials were derived from Cheneai Group. Ore fluid is the descending meteoric water-formed hot brine which were driven by structure and heat source to circulate and leach out Au, Ag and other ore-forming material from Chencai Group and emplaced in the ore-locating structural space through F_1 fracture and the like.
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