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THE DETERMINATION OF THE BEIJIANGJUN LITHOLOGIC ASSOCIATION IN THE FUCHASHAN AREA, MIDDLE ANHUI AND ITS IMPLICATIONS

XU Wei ;TONG Jin-song;HU Hai-feng ;WANG You-sheng ;CHEN Xiu-qi (Department of Resources and Environment Sciences, Hefei University of Technology, Hefei 230009, China ; Academy of Geological survey of Anhui Province, Hefei 230009, China)  
The southward extension of the Fuchashan area in Middle Anhui is represented by the section around the Dahuangshan Mt. where a suite of substantially unmetamorphosed strata are outcropped. Based on integrated analysis of rock association, meta- morphic degree, microfossils, it is regarded as the Beijiangjun lithologic association which can be correlated with the Zhangbaling area and subdivided into two lithologic members, i. e. the lower member of carbonate rock and the upper one of fragmental rock.
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