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中文摘要: 南仇铁矿床位于鲁西临淄境内，为小型褐铁矿矿床。矿体以层状或似层状为主；矿体规模较小，厚度、品位变化较大；褐铁矿矿石自然类型以致密块状、蜂窝状、粉粒状几种矿石较普遍。断裂构造和围岩对成矿、控矿具有重要的作用，矿体以交代作用为主。矿床成因属中低温热液交代充填—风化淋滤型矿床。沿层间及深部均有较好的找矿前景。
中文关键词: 褐铁矿矿床 地质特征 矿床成因 中低温热液交代充填—风化淋滤型 山东临淄
Abstract:Nanchou iron deposit is a small limonitel deposit in Linzi, western of Shandong province. The form of orebody is bedded or stratoid vein. The mass of ore is a small size orebody which vary in thickness and grade. The main natural type of limonite ore includes massive, honeycomb and pulverulent. The fault structure and wall rock are important in mineralization and ore-controling factor. The deposit is a middle-low hydrothermal type deposits related to metasomatic filling-weathering and leaching processes. The interlayer and deep location of the main fault structure have preferable prospect of limonite exploration.
keywords: limonite deposit geological characteristics deposit origin Middle-low Hydrothermal Related to Metasomatic Filling-Weathering and Leaching Type Linzi, Shandong province
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周 军?,葛 均,段红梅.南仇铁矿地质特征及矿床成因[J].有色金属（矿山部分）,2011,63(1):36-41.
ZHOU Jun,GE Jun,DUAN Hongmei.Geological Characteristics and Deposits Origin of Nanchou Iron Deposit[J].NONFERROUS METALS(Mining Section),2011,63(1):36-41.
周 军?,葛 均,段红梅.南仇铁矿地质特征及矿床成因[J].有色金属（矿山部分）,2011,63(1):36-41.
ZHOU Jun,GE Jun,DUAN Hongmei.Geological Characteristics and Deposits Origin of Nanchou Iron Deposit[J].NONFERROUS METALS(Mining Section),2011,63(1):36-41.
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