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《Guizhou Geology》 1989-01
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A Discussion on the Origin of Zhijin Cavern and the U Isotope Age Measurement

Fu Zhichong ( No. 1 Geological Team of Hydro-engineering, Guizhou Bureau of Geology and Minerals ) Jia Shuyan, Xia Xianming Peng Xiufeng ( Chengdu College of Geology ) ( Sichuan University )  
The authors of this article have been to Zhijin Cavern for several times to make investigatons and have collected eight geological samples. The U isotopic geological age measurement of the samples were separately made. Based on the measurement results and according to the geological and hydrogeological conditions in that region, the authors deal with the origin mechanism and models of some important rocks of Zhijin Cavern in this article. The development of the form of Zhjjin Cavern can be divided into two main stages: the early stage of the horizontal cavern development and the late stage of the funnel-like cavern development. The appearance of the latter karst development stage is in relation to the structural formation of carbonate rock strata and the new structural movement of the intervallic rise of Yunnan-Guizhou Plateau, showing continuing development characters of palaeokarst water nets. But the formation of those special stones of the cavern are in relation to the development of the special funnel-like cavern.
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