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.
出处
《安徽地质》
2001年第1期19-23,共5页
Geology of Anhui
关键词
北将军(岩)组
对比
皖中浮槎山地区
Beijiangjun rock association
correlation
Fuchashan area
Middle Anhui
