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;

The Huanggoushan Pb Zn deposit,occurring in the dolomite marble of Mesoproterozoic Zhenzhumen formation,is obviously controlled by strata.

WT5BZ]Guigang pingnan Pb Zn deposit is a complex type of polymetallic ores with a main origin of hydrothermal deposition and transformed by structure activties and hot water from magma, and it is controlled by a series of NNE SSW striking anticlines (fractures) and synclines.