【摘要】 清流仁场铅锌银矿是受推覆构造和层位双重控制的热液矿床 ,已控制矿体的赋存位置有明显的规律性 ,大致分布于“S”形的中部破碎带较厚的部位 ,由于断裂面产状变化引起的局部张性环境有利于热液交代和充填所致。根据这一观点 ,相应的构造位置就是今后的找矿靶区。更多还原

【Abstract】 The Renchang lead-zinc-silver deposit is a hydrothermal deposit which is con tro lled by nappe structures and stratigraphic position The distribution of proba b le orebodies has an obvious regular pattern The ore bodies are almost always discovered in the thicker part of the center section of the S-shaped ruptur ed zone The local tension circumstance resulted from the occurrence of ruptured surfaces is favourable to hydrothermal replacement and filling On this view, t he corresponding structural location is a prospecting target in the future ore- finding work更多还原