摘要
山东省烟台市牟平区辽上金矿床位于郭城断裂带东侧 ,赋存于荆山群野头组大理岩与震旦期花岗岩之接触带附近 ,矿体受NE向次级构造裂隙控制 ,呈盲矿体产出。
Liaoshang gold deposit in Muping of Shandong, located in east side of Guocheng fults occurs near the contact zone between the marble of Yetou formation of Jingshan group and the granites of Sinian.The orebodies controlled by suborder structures occur as blind ones.
出处
《山东地质》
2000年第3期22-25,共4页
Geology of Shandong
关键词
热液型金矿
隐伏矿体
山东
辽上金矿
地质特征
Gold deposit of hydrothermal type
Blind orebody
Economic geology
Muping in Shandong
