From north to south, the Silurian lead-zinc deposits in this area can be divided into 3 mineralized zones, they are Sirengou-Nanshagou lead-zinc mineralized zone, Hongtupo-Hanshigo.

Geological and metallogenic characteristics of Liushutang lead-zinc deposit are invested to reveal regularity and genesis of this deposit,which is trending to the south and forming by magma hydrothermal fluid.

Identification and study of stockwork altered pipe of Xitieshan lead-zinc deposit,Qinghai Province;

MORPAS-based multi-information prognosis of lead-zinc deposits in Lintan-Dangchang area, Gansu Province;

Geological-geochemical characters and genesis of the Heshuxia lead-zinc deposit, Guangdong Province;

Geological characteristics of the Tonglushang Pb-Zn deposit with its prospecting direction,Northwestern Guizhou;

Mineralization characteristics and ore-forming mechanism of the Jianbidong Pb-Zn deposit in Fengshun County,Eastern Guangdong;

Geological characteristics and genesis of the Weibao Pb-Zn deposit in Ruoqiang County,Xinjiang;

The paper summarized the geological cognition of the fomer reseachers on the ore-controlling structure,orebody occurrence characteristics and deep part ore prospecting perspective of the Maomaochang-Zhazichang lead-zinc deposit in Northwestern Guizhou.

Skarn and mesothermal-epithermal fluid filled lead-zinc deposits were found outside the molybdenum deposit during recent years' survey of land and resources,which occur in ring belt surrounding the Nannihu molybdenum deposit.

Geological characteristics of Tianshengguan Pb-Zn ore deposit;

With study on the geological settings, ore-forming conditions, deposit geology and tectono-geochemistry of Hetaoping Pb-Zn ore deposit, some acknowledgements have been attained as following: (1) Structures, strata and rocks are the ore-controlling factors;O.

Polygenetic compound mineralization of Fankou Pb-Zn ore deposit, Guangdong;