澜沧县看马山铁矿床分布在“三江”地区南段的临沧花岗岩基南端两侧.铁矿体呈层状、似层状产出.该铁矿的形成和分布受层位、岩性建造、火山-沉积旋回等综合因素的控制,属于典型的火山喷发沉积—变质矿床.地层岩性和航磁异常是寻找该类型铁矿床的重要标志.%Kanmashan iron ore deposit in Lancang county is located near Lincang granite of south of " Three River" mineralization area. Ore body of the Fe deposit is layered and appear to be a layered . Mineralization and distribution of the iron deposit is controlled by comprehensive factors such as stratigraphic layer, rock construction and volcanic-sedimentary cycles. The deposit is a typical volcanic eruption sedimentary-metamorphic deposit. The stratigraphic lithology and aeromagnetic anomaly is a important sign to prospect this type of iron deposit.
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