摘要
The Hadamengou gold deposit, located 15 km west of Baotou city, Inner Mongolia （Fig. 1）, contains deep-seated faults and a large granite body. The deposit is hosted by the Neoarchean Wulashan Group metamorphic strata.
The Hadamengou gold deposit, located 15 km west of Baotou city, Inner Mongolia （Fig. 1）, contains deep-seated faults and a large granite body. The deposit is hosted by the Neoarchean Wulashan Group metamorphic strata.
