摘要
normal; ORPHANS: 2; FLOAT: none; LETTER-SPACING: normal; COLOR: rgb(36,36,36); WORD-SPACING: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px"> normal; ORPHANS: 2; LETTER-SPACING: normal; COLOR: rgb(36,36,36); WORD-SPACING: 0px; PADDING-TOP: 0px; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px" id=EnChDivSummary name="EnDivSummary">In this paper, the authors studied the metallotectonic environment, ore-bearing formation and geochemistry of the greenstone belt iron-phosphate deposits in the northern margin of the North China platform. The result shows that the island arc-chlorite is the main native rock, and the post metamorphic host rocks belong to alkali- ferruginous and femic series. By analogy with the present exploitation situation of the low-grade endogenetic iron-phosphorite deposits in north China, there will be a good prospect of comprehensive utilization of greenstone belt iron-phosphate deposits in the northern margin of the north china platform.