皖中浮槎山地区北将军(岩)组的确定及其意义  

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

作　　者：许卫[1] 童劲松[1] 胡海风[1] 王有生[1] 陈秀其[1] 

机构地区：[1]安徽省地质调查院

出　　处：《安徽地质》2001年第1期19-23,共5页Geology of Anhui

摘　　要：皖中浮槎山地区南延部分以大黄山一带为代表，出露一套基本未变质地层，据岩石组合、变 质程度、微古化石等特征综合分析，认为其应为北将军（岩）组，可与张八岭地区的北将军（岩）组进行对 比，进一步将其分为两个（岩）段：下（岩）段为碳酸盐岩，上（岩）段为碎屑岩。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.

关 键 词：北将军(岩)组 对比 皖中浮槎山地区 

分 类 号：P588.24[天文地球—岩石学] P588.21[天文地球—地质学]