摘要
A certain gold deposit in eastern Liaoning province is located on the northern margin of North China platform, eastern Liaoning massif of mid-part of Tieling-Jingyu ancient uplift, which is double controlled by northeast-striking Hunhe and Suzihe fracture. Archeozoic granite-greenstone provided original source layer for mineralization and Mesozoic magma activity provided hot source and brought ore-forming matter, causing ore elements activation, transformation, localization and the formation of the gold deposit in eastern Liaoning.