云南省个旧地区把南组地层岩性对比探究
운남성개구지구파남조지층암성대비탐구
Lithology Comparison Analysis of Banan Formation in Gejiu Area of Yunnan
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    2014年 29期 291-293 ,共3页

    杨栋%赵云江%都鹏飞

    양동%조운강%도붕비

    云南个旧%剖面%岩性%对比 雲南箇舊%剖麵%巖性%對比
    운남개구%부면%암성%대비
    Gejiu,Yunnan%profile%lithology%comparison
    本文通过新测制个旧地区把南组（T3b）剖面（共计2900米）与云南省地质局1970年测制的鸟格组（T3n）剖面的对比发现，认为鸟格组地层应归属到把南组地层内，而把南组地层岩性显示为浅海相，沉积方向由上层至下层。
    본문통과신측제개구지구파남조（T3b）부면（공계2900미）여운남성지질국1970년측제적조격조（T3n）부면적대비발현，인위조격조지층응귀속도파남조지층내，이파남조지층암성현시위천해상，침적방향유상층지하층。
    In this article, through comparing the new measured Banan Formation (T3b)profile (2900 meters in total) in Gejiu, Yunnan with the Niaoge Formation (T3n) profile measured by geological survey in yunnan province in 1970, this paper found that Niaoge Formation belonged to the Banan Formation, and the lithology of Banan Formation layer showed a neritic facies, sedimentary direction from upper to lower.
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