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沂水县南仉林钛、铁矿地质特征
引用本文:周长祥,马晓东,刘鹏瑞,彭庆吉,张春法.沂水县南仉林钛、铁矿地质特征[J].山东地质,2008(12):21-23.
作者姓名:周长祥  马晓东  刘鹏瑞  彭庆吉  张春法
作者单位:山东省地质科学实验研究院,山东济南250013
摘    要:沂水县杨庄南仉林钛、铁矿位于沂沭断裂带汞丹山凸起的东南部,矿体为含磁铁矿钛铁矿角闪石岩,围岩为新太古代晚期第三阶段弱片麻状中粗粒二长花岗岩。矿区圈定钛、铁矿体1个,呈脉状产出,较规则,总长度约1200m,宽25—67m,平均40.3m,延深大于200m。矿体平均品位rife20.13%,Ti028.86%。属晚期岩浆分异型钛、铁矿床。

关 键 词:  铁矿  矿床地质  成矿条件  南仉林  山东沂水

Geological Characteristics of Titaninum and Iron Deposit in Nanzhanglin of Yishui County
Institution:ZHOU Chang - xiang, MA Xiao -dong, LIU Peng - rui, PENG Qing - ji, ZHANG Chun - fa (Shandong Institute and Laboratory of Geological Sciences, Shandong Jinan 250013, China)
Abstract:Nanzhanglin titanomagnetite deposit in Yangzhuang village of Yishui county locates in southeast of Gongdanshan uplift in Yishu fault belt. Its orebodies are titanomagnetite - bearing hornblende rock, while its country rocks are weak gneissic coarse - medium grain granite in the third phase of late period of Neoarchean. One titanomagnetite orebody has been circled in this mine area, which occurred in vein type regularly. The total length of this orebody is about 1200m, the width is 25 - 67m, the average width is 40.3m, and its extension depth is over 200m. Among the average grade of orebody, the TFe is 20.13% and TiO2 is 8.86%. It belongs to late period of magmatic differentiation type titanomaguetite deposit.
Keywords:Titanomagnetite  deposit geology  ore - forming condition  Nanzhanglin  Yishui in Shandong province
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