摘要
八里桥铅锌银矿位于将乐—宁化钨锡多金属成矿带东北侧,产于燕山早期第三阶段第三次侵入的中粒黑云母花岗岩外接触带上,贮存于早三叠世溪口组矽卡岩中。矿体呈似层状、透镜状产出,属热液充填型脉状铅锌银矿床。
The Baliqiao lead-zinc-silver deposit is located at the northeast side of the Jiangle-Ninghua tungsten-stannum polymetallic metallogenetic belt,exists in the exocontact belt of mesograin biotite-granite intruded in the early Yanshanian stage and in the skarn of early Triassic Xikou Formation strata.The orebody is discovered in parabedded or lenticular forms.It belongs to the veiny lead-zinc-silver deposit of the hydrothermal filling type.
出处
《福建地质》
2011年第1期12-16,共5页
Geology of Fujian
关键词
铅锌银多金属矿床
地质特征
成因探讨
将乐八里桥
lead-zinc-silver polymetallic deposit
geological characteristics
discussion of the genesis
Jiangle County