Ore structures of Xieziding gold deposit in Penglai city are faults with the trend of NW. Compressoshear faults with the trend of NW and its derived fault fissure system are important structure symbols of gold occurrence space in this gold deposit. Potassium, silicification and pyritization sericitization are direct prospecting marks. Based on geological characteristics of the deposit, it is believed that the deposit belongs to low temperature of magmatic hydrothermal filling altered type gold deposit.