Regional occurrence of saline, mineralising fluids at the eastern border of the bohemian massif

机译：波希米亚地块东部边界的盐分，矿化液区域性出现

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Several recently discovered post-Variscan Pb-Zn mineralisations in Devonian and Lower Car-boniferous limestones of the Bohemian Massif have been investigated. The mineralising fluids were low temperature (T_H=41 deg-103 deg), saline (12.1-23.4 eq.wt

机译：研究了波西米亚地块的泥盆纪和下碳统石灰岩中的一些最近发现的瓦里斯坎后铅锌矿化。矿化液是低温（T_H = 41 deg-103 deg），盐水（12.1-23.4 eq.wt

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《Biennial SGA meeting;Quadrennial IAGOD symposium》|1999年|p.901-904|共4页
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M.Slobodnik; Ph.Muchez; Z.Dolnicek; L.Zak;
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4. Regional occurrence of saline, mineralising fluids at the eastern border of the bohemian massif [C] . M.Slobodnik, Ph.Muchez, Z.Dolnicek, Biennial SGA meeting . 1999

机译：区域发生盐水，波希米亚东部边界的矿物质流体
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Regional occurrence of saline, mineralising fluids at the eastern border of the bohemian massif

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