The ore body of the Chikeng fluorite mine in Qingliu county is mainly in the form of large veins and long lenses,occurring in the northeast trending fault zone of fragmented porphyritic medium coarse grained syenogranite.This fault zone is both a mineral conducting structure and a mineral storing structure,and its ore body morphology and occurrence are strictly controlled by the fault.Based on this,analyze the geological characteristics and genesis of the Chikeng fluorite mine in Qingliu county.
关键词
萤石矿/地质特征/矿床成因/清流县
Key words
fluorite/geological characteristics/genesis of deposit/Qingliu county
维普
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