陈一笠. 1992: 天津市蓟县发现沉积型海泡石矿床. 地质通报, (3): 204-210.
    引用本文: 陈一笠. 1992: 天津市蓟县发现沉积型海泡石矿床. 地质通报, (3): 204-210.
    CHEN Yi-li. 1992: THE DISCOVERY OF A SEDIMENTARY SEPIOLITE DEPOSIT IN JIXIAN,TIANJIN MUNICIPALITY. Geological Bulletin of China, (3): 204-210.
    Citation: CHEN Yi-li. 1992: THE DISCOVERY OF A SEDIMENTARY SEPIOLITE DEPOSIT IN JIXIAN,TIANJIN MUNICIPALITY. Geological Bulletin of China, (3): 204-210.

    天津市蓟县发现沉积型海泡石矿床

    THE DISCOVERY OF A SEDIMENTARY SEPIOLITE DEPOSIT IN JIXIAN,TIANJIN MUNICIPALITY

    • 摘要: 通过1:5万区调工作,首次在天津蓟县地区发现海相沉积型海泡石矿层,这是本区在找矿方面的一个突破,海泡石矿赋存在蓟县系雾迷山组八段中一上部,含矿岩系厚约35m、层位稳定。二个矿层厚度分别为1.91m、2.21m,海泡石平均含量分别为25.6%、13.8%。形成环境属于浅海—滨海的碳酸盐台地。

       

      Abstract: A marine sedimentary sepiolite deposit was for the first time discovered in Middle and Upper Proterozoic strata in the Jixian area of Tianjin Municipality through. 1:50000 regional surveys. This is a major breakthrough in mineral prospecting in this area. The sepiolite deposit occurs in dolomite of the middle-upper part of the 8 th member of the Wumishan Formation of the Jixian System, yielding abundant stromatolites. The ore-bearing rock series. 35 m thick, is stratigraphically peisistent. This deposit includes two ore beds, which respectively are 1.91m and 2.21 m thick and have average grades of 25.6% and 13.%%. The ore-bearing dolomite was formed in an environment of neritic-littoral carbonate rock platforms.

       

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