Space-time and origin of the gold veins in the ore field were closely related with some lamprophyre dykes.

Metallogenic evolution of Tuokuzibayi gold deposit in southern Altay,north Xinjiang:Evidence from characteristics of quartz vein systems,isotopic geochemistry and Ar-Ar chronology;

U-Pb isotopic determination by SHRIMP method for Zirconium in gold-bearing quartz veins of Zhaishang gold deposit in Gansu Province and its geological meaning;

Geochemical difference between quartz veins of two generations at the Tongchang porphyry copper deposit, Jiangxi Province;

Study on thermoluminescence characteristics of quartz veins and their gold potentiality at Shihu gold deposit in Western Hebei;

There are two types of scheelite ore (skarn type and quartz vein type) in the Nanyangtian scheelite deposit.

The quartz vein type gold deposits of xiaoqinling area are mainly distributed south to the Mesozoic granite batholiths such as Wenyu and Huashan and entirely hosted in Archean greenstone belt of Dangzchc group and early Proterozoic Khondalite series of Shuidigou group.

Saiwusu gold deposit in inner Mongolia is an auriferous quartz vein type.