摘要
贵州泥堡金矿和贵州水银洞金矿处于相同的大地构造背景中,同属滇黔桂"金三角"中有名的卡林型金矿,它们具有相似的控矿地层、构造,矿体的产出特征也有明显的可对比性。两个矿区的成矿都与龙潭组地层、sbt、背斜及断裂构造还有特定的围岩蚀变有密切的关系。对比研究两个矿区的特征发现,泥堡金矿和水银洞金矿为层位、构造、围岩蚀变相结合的"三位一体"成矿模式。
In the same geotectonic background, the Guizhou mudburg and Guizhou water silver cave gold deposits belong to the famous Karin type gold deposits in Yunnan Guizhou Guangxi "Golden Triangle". They have similar ore controlling strata and structures, and the output characteristics of the orebodies are also obviously contrastive. The mineralization in the two mining areas is closely related to the Longtan Formation, SBT, anticline, fault structure and specific wall rock alteration. By comparing the characteristics of the two mining areas, we find that the "Ni in Bao gold deposit" and "quicksilver gold deposit" are the Trinity metallogenic model combining stratigraphic, structural and wall rock alteration.
引文
[1]刘建中,刘川勤.贵州水银洞金矿床成因探讨及成矿模式[J].贵州地质,2005,22(1):9—14.
[2]刘建中,邓一明,刘川勤,等.贵州省贞丰县水银洞层控特大型金矿成矿条件与成矿模式[J].中国地质,2006,33(1):169—177.