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| 庐枞盆地龙桥铁矿床中菱铁矿的地质特征和成因意义 | |
| 引用本文： | 段 超,周涛发,范 裕,袁 峰,丁 铭,尚 世贵,张乐骏.庐枞盆地龙桥铁矿床中菱铁矿的地质特征和成因意义[J].矿床地质,2009,28(5):643-652. |
| 作者姓名： | 段 超 周涛发 范 裕 袁 峰 丁 铭 尚 世贵 张乐骏 |
| 作者单位： | 1. 合肥工业大学资源与环境工程学院,安徽,合肥,230009 2. 安徽省庐江龙桥矿业有限公司,安徽,巢湖,231555 3. 合肥工业大学资源与环境工程学院,安徽,合肥,230009;安徽省地质矿产局327地质队,安徽,合肥,230011 |
| 基金项目： | 国家重点基础研究发展规划973项目，高等学校博士学科点科研基金项目，国家自然科学基金项目，安徽省优秀青年科技基金项目( |
| 摘 要： | 龙桥铁矿床是庐枞火山岩盆地中的一个大型的铁矿床,多年来对其矿床成因的认识存在较大的争论.文章在野外地质研究工作的基础上,通过对矿床中菱铁矿的岩矿分析鉴定和电子探针测试,确定了矿床纹层状矿石中的菱铁矿为沉积成因.通过对菱铁矿的产出特征分析,并结合龙桥铁矿床的部分地质地球化学研究成果,认为在该矿床形成过程中,早期沉积形成了纹层状的菱铁矿层,在燕山期的岩浆热事件中,部分沉积菱铁矿被交代形成了磁铁矿和具有残余骸晶结构等一系列矿石交代组构特征的矿物.纹层状矿石既具有沉积特征,也具有热液改造特征,证实了矿床的形成存在早期(三叠纪)的沉积成矿(菱铁矿)作用和晚期(燕山期)的热液成矿(磁铁矿)作用.菱铁矿的研究为进一步确定龙桥铁矿床的成因提供了新的佐证. |
| 关 键 词： | 地质学 庐枞火山盆地 龙桥铁矿床 菱铁矿 矿床成因 |
Geological characteristics of siderites from Longqiao iron deposit in Luzong volcanic basin and their genetic significance |
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| DUAN Chao,ZHOU TaoFa,FAN Yu,YUAN Feng,DING Ming,SHANG ShiGui,ZHANG LeJun.Geological characteristics of siderites from Longqiao iron deposit in Luzong volcanic basin and their genetic significance[J].Mineral Deposits,2009,28(5):643-652. | |
| Authors: | DUAN Chao ZHOU TaoFa FAN Yu YUAN Feng DING Ming SHANG ShiGui ZHANG LeJun |
| Abstract: | The Longqiao iron deposit is one of the most important large ore deposits in Luzong basin, one of the ore-concentrated area in the Middle and Lower Yangtze Valley metallogenic belt. The genesis of this ore deposit remains a problem of much controversy. Based on careful and detailed field investigation and mineral association research, this paper has reported some new achievements concerning siderite minerals in this deposit. There exist two types of siderites in the ores: one occurs in the lamellar ores, and the other assumes the veined form. Petrographic and electron probe analyses as well as C-O, H-O isotope geochemical characteristics of the siderites in the lamellar ore all show that siderites of this kind were formed earlier than magnetite and other minerals associated with magnetite, and that they occurred in a marine sedimentary environment. Some siderites were transformed into magnetite by later hydrothermal activities, resulting in the formation of residual and metasomatic textures in the ores. The lamellar iron ores are composed of sedimen-tary siderite and hydrothermal minerals such as magnetite, garnet, pyrite and phlogopite as a result of the water-rock interaction be-tween the hydrothermal fluids evolved from the Mesozoic magmatic intrusion and the siderite-beating Early Mesozoic (Middle Trias-sic) marine sedimentary rocks. Most of the magnetites in the ore deposit, espeeiaUy in the massive iron ores, were precipitated direct-ly from the magmatic water-dominated hydrothermal system. The metallogenic process of the Longqiao iron deposit can be divided in-to the early (Middle Triassic) sedimentary ore-forming stage characterized by the deposition of siderite-beating rocks and the late (Early Cretaceous or Yanshanian) hydrothermal ore-forming stage characterized by the formation of magnetites associated with other hydrothermal minerals. |
| Keywords: | geology Luzong volcanic basin Longqiao iron deposit siderite genesis of ore deposit |
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