平度市新河铁矿地质特征及找矿远景  

Geological Characteristics and Prospecting Perspective of Xinhe Iron Deposit in Pingdu City

作　　者：张吉涛 马健 

机构地区：[1]山东省第四地质矿产勘查院,山东潍坊261021

出　　处：《山东国土资源》2016年第5期37-40,共4页Shandong Land and Resources

摘　　要：平度市新河铁矿处于莱州-安丘铁成矿带中部,矿床赋存于古元古代粉子山群小宋组二段含铁岩系中,属沉积变质型铁矿床。通过地质勘查,矿区内圈定3个铁矿体。该文以此为基础,对矿床地质特征及矿区找矿远景进行浅析,以利于矿山下一步找矿工作的开展。Xinhe iron deposit locates in middle part of Laizhou-Anqiu iron ore belt in Pingdu city. The deposit occured in the second section of Fengzishan group. It belongs to sedimentary metamorphic type deposit. Through geological exploration,three iron ore bodies have been circled in the mine. On this basis,geological characteristics and prospecting perspective of this mine area have been analyzed. It will help the next step prospecting work.

关 键 词：铁矿 地质特征 粉子山群小宋组 找矿远景 平度市新河 

分 类 号：P618.31[天文地球—矿床学]