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长江中下游地区是我国重要的铁铜矿产基地,是环太平洋成矿带的一个组成部分,区域中成矿现象复杂并具有特色。多年来,各部门的地质工作者在本区进行过大量的地质勘查和研究工作,逐步加深了对区域地质特征和矿床成因的认识,并查明了相当丰富的铁、铜储量,促进了社会主义建设的发展。
The middle and lower reaches of the Yangtze River is an important iron-copper mineral base in China and an integral part of the Pacific Rim metallogenic belt. The regional mineralization is complicated and unique. Over the years, various departments of geological workers conducted a large number of geological prospecting and research work in this area, gradually deepening their understanding of the regional geological characteristics and the genesis of the deposit, and identified a considerable amount of iron and copper reserves and promoted social The development of doctrine construction.