The majority of orebodies locate in fractured pelitic and silty phyllites,with a minority in the pre-ore Indosinian granite-porphyry dykes or their contact zones,suggesting that the Indosinian granite magmatism was not,as interpreted in previous studies,the dominant factor to cause gold mineralization.

Zircon SHRIMP U-Pb dating of monzogranite-porphyry dikes in Shengongcun, northern Zhejiang, and its geological implications;

A study on basic geological characteristics of the granite porphyry dike swarm in Jianjianling shows that a large - scale granite porphyry body of high copper ore potential is possibly concealed underneath.

The measurement and application of joint roughness coefficient for rock mass of granite;