The geological characteristic of tungsten-gold deposits of Gaohe

Shaanxi Provence was described briefly. The metallogenic regularity from several aspects was discussed

such as faults

lithology

mineralization enrichment

hydrothermal activity

geophysical and geochemical anomalies. and considered that the north-east fracture structure of Dongjiangkou rock control the concentration distribution of ore（mineralized） belt

point

and also considered that tungsten-gold deposits directly exist in the fracture structure as well as the second grade. Dykes

quartz veins or the others are the directly sign of prospecting.