摘要
///The metallogenetic zone of Xiangtu Pb-Zn multimetallic deposit is in the Sanhedong Formation (T3s)limestone and the interlayer fracture zone of the contact between the top limestone and Waluba Formation (T3wl)lamellted mudstone. The 3 Fe, Pb, Zn metallogenetic bodies belong to the Pb, Zn (Fe) deposit of structure fracture zone type, formed by sedimentation and reformation.