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    张开毕, 陈金良, 林亨才, 黄昌旗, 罗志兴. 闽西南地区南华纪—震旦纪岩石地层的划分与对比[J]. 中国地质, 2005, 32(3): 363-369.
    引用本文: 张开毕, 陈金良, 林亨才, 黄昌旗, 罗志兴. 闽西南地区南华纪—震旦纪岩石地层的划分与对比[J]. 中国地质, 2005, 32(3): 363-369.
    ZHANG Kai-bi, CHEN Jin-liang, LIN Heng-cai, HUANG Chang-qi, LUO Zhi-xing. Lithostratigraphic division and correlation of the Nanhuaan-Sinian Periods in southwestern Fujian[J]. GEOLOGY IN CHINA, 2005, 32(3): 363-369.
    Citation: ZHANG Kai-bi, CHEN Jin-liang, LIN Heng-cai, HUANG Chang-qi, LUO Zhi-xing. Lithostratigraphic division and correlation of the Nanhuaan-Sinian Periods in southwestern Fujian[J]. GEOLOGY IN CHINA, 2005, 32(3): 363-369.

    闽西南地区南华纪—震旦纪岩石地层的划分与对比

    Lithostratigraphic division and correlation of the Nanhuaan-Sinian Periods in southwestern Fujian

    • 摘要: 提要:福建西南部长汀、上杭一带广泛发育一套海相砂、泥质及硅质沉积的浅变质岩系,经过1∶25万瑞金市幅区域地质调查,在证实“丁屋岭砾岩”的时代为晚泥盆世而从浅变质岩系中划分出去后,笔者将整合于早—中寒武世林田组之下的浅变质岩系,自下而上划分为姜畲坑组、赖坑组、南岩组和黄连组。

       

      Abstract: Abstract:A low-grade metamorphic series composed of marine sandy, muddy and siliceous sediment is widespread in Changting and Shanghang, southwestern Fujian. According to the regional geological survey of the 1:250000 Ruijin Sheet, the “Dingwuling conglomerate” is determined to be of Late Devonian age and thus separated from the low-grade metamorphic series. In this paper, the low-grade metamorphic series that conformably underlies the Lower-Mid Cambrian Lintian Formation is divided into the Jiangshekeng Formation,Laikeng Formation,Nanyan Formation and Huanglian Formation.

       

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