A study of regional geological setting and ore-control factors for the Xiasai Ag-Pb-Zn deposit indicates that NW-trending structures act as conduits for ore fluids and orebodies are controlled by a NNw-trending fault system, while ore shoots are confined equidistantly to secondary structures associated with the NNW-trending fault system.

Geologic features,ore-hunting indicator of the Deerbuer Ag-Pb-Zn deposit;

Petrochemistry and Sr, Nd isotopes of intrusive in Lengshuikeng porphyry type Ag-Pb-Zn deposit;

Relationship between fluid inclusions and ore-forming of Jiawula Ag-Pb-Zn deposit in Hulunbeir league,Inner Mongolia

The Bajiazi lead-zinc-silver deposit bears similar feature.

Many Pb-Zn-Ag deposits are found in the middle north margin of North China Block.

Four types of Pb-Zn-Ag deposits occur in the middle north margin of North China Block.

This paper presents an analysis of objective attributes in geology,geochemistry,and geophysics that occur in different sequences of the known mineral deposits,and of the metallogenic geological attributes in the Pb-Zn-Ag deposits in the northem Hebei Province.

Yingfang Pb-Zn-Ag deposit lies in a S-N direction medium ductile shear zone,its mainore body occurs in the contact zone between coarse Or-granite of early Yanshanian andHongqiyingzi Group of Lower Proterozoic.

Shidonggou Pb-Zn-Ag deposit exists within the external contact zone of Yeniutan granodiorite in-trusive,and is controlled by Shidonggou faulted structure.

Sulfur and lead isotopic compositions of lead-zinc-silver deposits in the Gangdise metallogenic belt, Tibet, China, and its geological significance.;

Potash micatization is one of the main hydrothermal alteration minerals genetically related to the lead-zinc-silver deposit.

In recent years, many large-medium scale lead-zinc-silver deposits were found in the southmargin of North China Craton such as Shagou, Lengshuibeigou, Laodaizhanggou and so on.