Root zone processes for the formation and evolution of a large-scale granitic batholith:drip structures,potassic volcanism and Earth surface processes;

Characteristics and tectonic setting of the Tula aluminous A-type granite at the south side of the Altyn Tagh fault, NW China.;

Recognition of the A-type granites from the Huangling granite batholith in western Hubei;

SHRIMP U-Pb zircon dating of Triassic A-type granites in Sonid Zuoqi,central Inner Mongolia,China,and its tectonic implications;

Characteristics and tectonic setting of Middle-Permian A-type granites in Tianshuijing area, west of Inner Mongolia;

The Mesozoic A-type granites are widely developed in southeastern China.

Detiled field geological mapping and geochemical study show that the Fuling rock mass in southern Anhui is enriched in Si ,Al,alk , high-field strength elements ,REE ,Rb and depleted in Sr and Ba,belonging to aluminous A-type granites.

SHRIMP U-Pb zircon dating of the Dushan granitic batholith and related granite-porphyry dyke, eastern Hebei Province,;

The Dangchuan granitic batholith,which is located in the conjunction area of the Qilian and the North Qinling orogenic belts,is composed of 9 granitic intrusive bodies,whose rocks are rich in K_2O generally.

Located in the area of the Qilian and west Qinling orogenic belts,the Dangchuan granitic batholith is composed of 9 granitic intrusives.