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莱芜市独路石墨矿矿床地质特征及矿床成因
引用本文:李雷,赵体群,周广海,李世达,柳清丽,王强,张相峰,李鹏辉,蒋波,沙启文.莱芜市独路石墨矿矿床地质特征及矿床成因[J].山东地质,2013(10):27-30.
作者姓名:李雷  赵体群  周广海  李世达  柳清丽  王强  张相峰  李鹏辉  蒋波  沙启文
作者单位:[1]莱芜市国土资源局,山东莱芜271100 [2]山东省第一地质矿产勘查院,山东济南250014
摘    要:独路石墨矿位于泰山一沂山断隆泰山凸起东端,矿床赋存于新太古代泰山岩群雁翎关组之中。矿床内发育6个石墨矿体,呈层状、似层状产出。矿石类型主要为含石墨黑云变粒岩型,石墨矿石属鳞片状晶质石墨矿,石墨矿物片径细小。矿石样品固定碳含量一般为6%~8%,在省内属较高品位。原岩为富含有机质的杂砂岩——沉积凝灰岩,经中低压变质相系变质作用形成石墨矿,属沉积变质成因。找矿标志明显,外围及深部找矿前景良好。独路石墨矿的发现填补了鲁西地区石墨矿空白。

关 键 词:独路石墨矿  地质特征  矿床成因  找矿标志  山东莱芜

Geological Characteristics and Origin of Dulu Graphine Deposit in Laiwu City
LI Lei,ZHAO Tiqun,ZHOU Guanghai,LI Shida,LIU Qingli,WANG Qiang,ZHANG Xiang feng,LI Penghui,JIANG Bo,SHA Qiwen.Geological Characteristics and Origin of Dulu Graphine Deposit in Laiwu City[J].Geology of Shandong,2013(10):27-30.
Authors:LI Lei  ZHAO Tiqun  ZHOU Guanghai  LI Shida  LIU Qingli  WANG Qiang  ZHANG Xiang feng  LI Penghui  JIANG Bo  SHA Qiwen
Institution:1. Laiwu Bureau of Land and Resources, Shandong Laiwu 271100, China; 2. No. 1 Exploration Institute of Geology and Mineral Resources, Shandong Jinan 250014, China)
Abstract:Dulu graphite mine locates in east part of Taishan--Yishan uplift. Deposit occurs in Yanlingguan formation of Archean Taishan group. Six graphite ore bodies developed in this deposit with layered and lstratiform--like types. Main types of ores are graphite--bearing biotite leptynite. Graphite ores belong to crystalline flake graphite deposit with small diameter. Fixed carbon contents of Ore samples are generally 6%-8%. It is a higher grade in Shandong province. Original rock is greywaeke rich in organic matter, that is sedimentary tuff. Through low--pressure metamorphic facies series metamorphism, graphite deposit has been formed. Its origin is sedimentary metamorphism with obvious prospecting symbol. Exploration prospect is good in its external and deep parts. The discovery of Dulu graphite deposit has filled the blank of graphite deposit in Luxi area.
Keywords:Dulu graphite deposit  geological characteristics  origin  Laiwu city in Shandong province
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