中国冶金地质总局三勘院在山西省盂县开展的一铁矿普查项目取得新进展,其深部发现新的铁矿体。该铁矿体产于超基性岩中,主要成分为橄榄石、磁铁矿,磁铁矿品位最高达32.22%,初步确定为岩浆晚期分异型矿床。根据目前取得的成果来看,该地区有望找到一处可供进一步勘查的中大型铁矿。 China Metallurgical Geology Institute of the three exploration in Yuxian County, Shanxi Province to carry out an iron ore census project made new progress, the deep discovery of new iron ore bodies. The ore body is produced in ultramafic rocks, the main component is olivine, magnetite, magnetite grade up to 32.22%, initially identified as late magmatic magmatic deposits. Based on the results achieved so far, the region is expected to find a large and medium-sized iron ore mine for further exploration.