莱州市大浞河铁矿矿床地质特征及找矿方向

Geological Characteristics and Oreprospecting Direction of Dazhuohe Iron Deposit in Laizhou City

摘要:

大浞河铁矿赋存在古元古代粉子山群底部的小宋组层间破碎带内，该组地层是矿床主要的矿源层。根据论证后的工业指标对矿床进行重新圈定及评价，并对矿床地质特征、主要控矿因素、矿体赋存规律及找矿标志进行浅析，以利于矿山地质找矿工作的开展。

Abstract:

Dazhuohe iron ore deposit are hosted in the interlayered fractured zone of XiaoSong formation at the bottom of FenZi mountain group in early Proterozoic Erathem. The formation is the major ore source bed. According to the industrial index demonstrated, the deposit is redelineated and reevaluated. This article also briefly explores the geological characteristics of the deposit, the main orecontrol factors, the occurrence regularity of ore body and ore prospecting marks in order to help prospecting work.