摘要
The Shagou iron deposit occurs mainly in marble of the Middle Devonian Qingshiya Formation,in which iron orebodies,featured in homogeneous distribution of components,appear in stratified and/or stratoid beds with the same attitude to the marble.Magnetic anomalies at both the east and west sides of the iron concession are large in scale,high in anomalous value and good in continuity,which provide a great potential for ore prospecting in this area.