摘要
沙沟铁矿主要赋存于中泥盆统青石垭组大理岩中,矿体规模大,呈层状、似层状,产状与大理岩一致,组分均匀。
The Shagou iron deposit occurs mainly in marble of the Middle Devonian Qingshiya For- marion, 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..
出处
《陕西地质》
2013年第1期7-12,共6页
Geology of Shaanxi
