Abstract：This deposit is one of important Ag deposits found recently in the north part of He-bei. In this paper basing on the work of predecessors and many geologic observtions of surface, producing area, drilling cores, from the genesis of siliceous breecia, the divide of ore-foroming stages, ore forming physio-chemical conditions, inclusion etc, authors discuss the genesis of this deposit and give a metallogenic model Ore-forming tempheratures of this deposit are relatively high (220 -350℃), metallogenic press are low (less than 260×105Pa), the depth is 0. 42-0. 86km, the forming environment is the subsurface environment, the ore-forming fluid is of characters of low salinity (less than 3. 35wt% NaCl), rich in K+, Cl-, F-, SO42-, poor in Na+, Ca2+, so it belongs to a typical hot spring type deposit.
刘凤山, 张国辉. 河北牛圈热泉型银(金)矿床成因[J]. 地质与资源, 1996, 5(1): 48-58.
Liu Fengshan, Zhang Guohui. GENESIS OF NIUJUAN HOT-SPRING TYPE Ag (Au) DEPOSIT IN HEBEI PROVINCE. GEOLOGY AND RESOURCES, 1996, 5(1): 48-58.
1996, Vol. 5 
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