Ore prospecting method for carbonate rock type lead-zinc ore deposit
A carbonate rock and carbonate mineral technology, applied in measurement devices, material analysis by electromagnetic means, instruments, etc., can solve relevant research gaps, lack of systematic research and comparison of carbonate minerals, no carbonate Minerals and other issues, to achieve the effect of realizing economy, high promotion and application value, and improving ore prospecting efficiency
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Embodiment 1
[0031] The macroscopic color characteristics of the carbonate mineral veins developed on the surface and tunnels of the lead-zinc deposits in Permian carbonate rocks in Hezhang County, Guizhou Province were classified, and the impure milky white calcite (RGB 248, 248, 255), off-white dolomite (RGB is 245, 245, 245), light red ferromanganese carbonate minerals (RGB is 255, 182, 193) are systematically collected according to the distribution, and the coordinates of the sampling points and Photograph;
[0032] The obtained carbonate mineral samples were observed for cathodoluminescence, and the carbonate minerals (RGB is 165, 42, 42 or 139, 0, 0) with cathodoluminescence with brownish red and deep red concentric rings were found, and detailed mineralogical observations;
[0033] Rare earth geochemical indicators: After field and indoor screening of calcite, conduct rare earth element geochemical analysis by solution method or LA-ICPMS in situ method, obtain rare earth element co...
Embodiment 2
[0037] The macroscopic color characteristics of the carbonate mineral veins developed on the surface and tunnels of the lead-zinc deposits in Carboniferous carbonate rocks in Huize County, Yunnan Province were classified, and the impure milky white calcite (RGB is 248 , 248, 255), off-white dolomite (RGB is 245, 245, 245), light red ferromanganese carbonate minerals (RGB is 255, 182, 193) are systematically collected according to the distribution, and the coordinates of the sampling points are marked and photographed;
[0038] The obtained carbonate mineral samples were observed for cathodoluminescence, and the carbonate minerals (RGB is 165, 42, 42 or 139, 0, 0) with cathodoluminescence with brownish red and deep red concentric rings were found, and detailed mineralogical observations;
[0039] Rare earth geochemical indicators: After field and indoor screening of calcite, conduct rare earth element geochemical analysis by solution method or LA-ICPMS in situ method, obtain ra...
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