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《Mineral Deposits》 1993-03
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MULTISTORY METALLOGENIC MODEL OF THE SHIZISHAN OREFIELD IN TONGLING,ANHUI PROVINCE

Huang Xuchen and Chu Guozheng (No. 321 Geological Parly, Anhui Bureau of Geology and Mineral Resources, Tongling, Anhui Province)  
More than ten ore deposits have been discovered in the Shizishan orefield, a major orefield in the iron-copper-sulfur-gold metallogenic belt of Middle and Lower Yangtze Valley. The orefield experienced a three-stage process of basement formation, stable cover deposition and intraplate deformation, i.e., it underwent very long tectonic evolution of active→stable→active, thus forming a complex geological setting. The ore-forming process resulted from the superimposition of Yanshanian magmatic activity on the Paleozoic-Early and Middle Triassic sedimentary formation and was conditioned by varied factors: proto reformed by the originally-deposited kappa-pyrite bed; the lithology favorable for metasomatic mineralization and the host bed and cover bed formed by favorable lithologic association; ore-forming materials and ore-bearing hot fluids provided by Yanshanian intermediateacid magma; well-developed wall rock alterations, consisting mainly of skarnization, potash alteration, silicification, chloritization, epidotization and sericitizations ore-forming fluids dominated by magmatic water at the early stage with the addition of formation water at the late stage; the superimpdsition of different types of structures that connected the magmatic source and provided favorable space for passage of ore fluids, and hosting of orebodies. The ore-forming process shows both endogenic and exogenic characteristics with a variety of mineralization types such as hydrothermal type, skarn type, stratabound skarn type and porphyry type, characterized by a distinct"vein-pipe-strata-porphyry"mineralization series with stratiform mineralization being most important. In section, this mineralization series exhibits a multistory form. Such a "a whole orebody composed of multilayered ores" type is to some extent typical in Tongling area and even in the whole Middle and Lower Yangtze Valley, thus having some guiding significance in ore-prospecting work of that region.
【Fund】: 国家“七五”重点攻关项目75-55-02-03的组成部分
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