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《Geology of Anhui》 2007-01
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DISCUSSION OF DIAGENETIC AND METALLOGENETIC BACKGROUND IN THE TONGLING AREA

CHEN Lin-jie,WU Duo-yuan,LIU Liang-gen(No.321 Geological Team of Bureau of Geology and Mineral Resources Exploration of Anhui Province,Tongling 244033,China)  
The Tongling area is one of the important mine clusters in the poly-metallic metallogenetic belt along the middle-lower Yangtze River reaches and is also one of the chief nonferrous metal bases in China.It is world-famous for its’ teeming with copper,gold and other mineral resources;especially the abundance of copper makes it enjoy the title of “copper land ”in China in ancient times.Ore deposit types in the area mainly include skarns,strata-bound skarns,and secondly,the small-sized porphyry at the depth of ore deposit(such as in Tongguanshan,Xinqiao,etc.).The mineralization is related to the extensive magmatic activities in the late Mesozoic(120-140Ma)[1,2] and the ore deposit is closely interrelated to intrusions both in space and time.The intrusions can be divided into alkaline and calc-alkaline series.They are the product of AFC process caused by underplating alkaline basaltic magma mixing with lower crustal dioritic magma,other than the product directly differentiated from alkaline basaltic magma.The tectonic setting is the extensional environment resulted from stretching of lithosphere.It is still possible to find out new hidden ore deposits in the Tongling area though the extent of research has been very high here.This paper aims to summarize the research results already made by geologists in the past and serve as a scientific basis for further exploration in the area.
【CateGory Index】: P618.2
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