期刊网首页  /  联系我们  /  English
高级检索
{{news.title}}

内蒙黄岗梁矽卡岩型铁锡矿床稀土元素地球化学

downloadPDF
文章导航 > 岩石学报 > 2002 > 18(4): 575-584

上一篇

下一篇

王莉娟 王京彬 等. 内蒙黄岗梁矽卡岩型铁锡矿床稀土元素地球化学[J]. 岩石学报, 2002, 18(4): 575-584.
引用本文: 王莉娟 王京彬 等. 内蒙黄岗梁矽卡岩型铁锡矿床稀土元素地球化学[J]. 岩石学报, 2002, 18(4): 575-584.
shu
WANG LiJuan 1,2,WANG JingBing 1,2,WANG YuWang 1,2,Hidehiko SHI MAZAKI 11. Research Center for Mineral Resources Exploration,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100101,China 2. Beijing Institute of Geology for Mineral Resources,Beijing 100012,China. REE geochemistry of the Huanggu angliang skarn Fe-Sn deposit, Inner Mongolia[J]. Acta Petrologica Sinica, 2002, 18(4): 575-584.
Citation: WANG LiJuan 1,2,WANG JingBing 1,2,WANG YuWang 1,2,Hidehiko SHI MAZAKI 11. Research Center for Mineral Resources Exploration,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100101,China 2. Beijing Institute of Geology for Mineral Resources,Beijing 100012,China. REE geochemistry of the Huanggu angliang skarn Fe-Sn deposit, Inner Mongolia[J]. Acta Petrologica Sinica, 2002, 18(4): 575-584.
shu

内蒙黄岗梁矽卡岩型铁锡矿床稀土元素地球化学

    • [1]中国科学院地质与地球物理研究所矿物资源中心，北京100101 [2]有色北京矿产地质研究所，北京100012

  • 基金项目:

    中科院 KZCX1 - 0 7课题，2 0 0 1 cb4 0 980 6项目联合资助

REE geochemistry of the Huanggu angliang skarn Fe-Sn deposit, Inner Mongolia

    摘要
  • 黄岗梁矿床是我国北方唯一的一处锡铁共生大型矽卡岩型矿床，苏大沟是黄岗梁矿床NE向延伸的铜铅锌矿点。黄岗梁矿床围岩、蚀变围岩、赋矿矽卡岩以及不同矿体石榴子石稀土元素的总特征体现了岩浆和岩浆水、围岩和大气降水对成矿的综合影响。靠近岩体则较多地体现了岩浆和岩浆热液作用；远离岩体则围岩地层和大气降水作用增强；从贫矿体－富矿体，从早阶段到晚阶段，大气降水对成矿的贡献增大，晚期又叠加了岩浆和岩浆热液成矿作用。黄岗梁铁锡矿床的REE配分曲线类型多样、变化较大，充分显示了成矿流体的多来源和多期次叠加成矿的稀土元素特征。苏木沟铜铅锌矿点具有岩浆热液稀土元素特征。稀土元素的研究初步建立了华北北缘黄岗梁式矽卡岩型矿床稀土元素配分模式。
    The Huanggangliang deposit is the large Fe-Sn paragenic one in northern China. The REE geochemistry of strata, altered rocks, ore-hosting skarn and garnet fro m various orebodies indicates that the comprehensive process of magma, magmatic water, wall rocks and especially meteoric water is responsible for metallization . The contribution of magmatism to metallization tends to increase toward intrus ive, but the contribution of strata and meteoric water to metallization tends to increase away from intrusive. The effect of meteoric water on metallization ten ds to be intensified from barren ore to rich ore. In the late stage, magmatic hy drothermal process was superimposed on metallization. The various REE patterns s ymbolize the multi-source of fluid and multi-phase metallization.The REE patte rns are the magmatic hydrothermal characteristics in Sumugou Cu-Pb-Zn deposit. The result of REE geochemistry primarily establishes the REE pattern model for the type of Huanggangliang skarn deposit.
    • HTML全文
  • 加载中
    • 参考文献(36)
  • [1]

    ［1］Chen Jun, Halls C, Stanley C J. 1994. The distrybutive feature and meaning of main rock-formation mineral of W, Sn, Mo, Bi skarn-deposit from Shizhuyuan area. Geochimica, 23(sup.):84-92 (in Chinese with English abstract)

    [2]

    ［2］Gressey G. 1987. Skarn formation between metachak and agglomerate in the central ring complex, Isle of Arran, Scotland. Mineral Mag., 51(2):231-246

    [3]

    ［3］Han Song, Huang zhongxiang, Jia Xiuqin. 1993. The geochemistry feature of REE elements of calcareous skarn and garnet from Gejiu Damoshan, Yunnan. Acta Petrologica Sinica, 9(2):192-197 (in Chinese with English abstract)

    [4]

    ［4］Li Hongbing, Wang Shijie, Li Chaoyang and Wen Jinming. 1997. REE and isotope(Sr,O) data for the evolution of ore-forming hydrothermal system: Evidence from the Baxi gold-skarn deposit in Songpan-Ganzi orogenic belt, Sichuan, China. Acta Mineralogica Sinica, 17(4): 412-421(in Chinese with English abstract)

    [5]

    ［5］Ling Qicong, Zhou Guibin, Huang Xuchen and Yan Yuqin. 1998. Mechanism and the characteristics of stratabound-type ore deposit. Journal of Procious Metallic Geology, 7(2): 91-95 (in Chinese with English abstract)

    [6]

    ［6］Mao Jingwen. 1987. On the characteristics of REE and its relationship with minerogenesis in BT tin mine, northern Guangxi autonomous region. Journal of Hebei College of Geology, 10(3):273-287 (in Chinese with English abstract)

    [7]

    ［7］Pan Jiayong, Zhang Qian, Li Caoyang. 2000. REE geochemistry of the Yangla copper deposit in western Yunnan. Acta Mineralogica Sinica, 20(1):44-49(in Chinese with English abstract)

    [8]

    ［8］Qiu Ruilong. 1987. The REE elements geochemistry from copper-skarn deposit in copper mountain, Guichi. Acta Geologica Sinica, 61(1):91-100 (in Chinese with English abstract)

    [9]

    ［9］Wang Guozheng. 1997. Geological characteristics and genesis of the Anle tin-copper deposit, Inner Mongolia. Mineral Deposits, 16(3):260-271(in Chinese with English abstract)

    [10]

    Wang Lijuan, Shimazaki H, Wang Jingbin, Wang Yuwang. 2001, Ore-forming fluid and metallization of the Huanggangliang skarn Fe-Sn deposit, Inner Mongolia. Science in China (Ser. D), 44(8):735-747

    [11]

    ［11］Wang Lijuan, Shimazaki H, Shiga Y. 2001. Skarns genesis of the Huanggang Fe-Sn deposit, Inner Mogolia, China. Resouce Geology, 51(4):359-376

    [12]

    ［12］Wang Lijuan, Wang Jingbin, Wang Yuwang, Mao Qian. 2001. Fluid-melt inclusions in fluorite of the Huanggangliang skarn iron-tin deposit and their significance to mineralization. Acta Geologica Sinica, 75(2):204-211

    [13]

    ［13］Wei L. 2002. Fluid-rock interaction during subsolidus microtextural development of alkali granite as exemplified by the Saertielieke pluton, Ulungur of the northern Xinjiang, China. Chemical Geology, 182: 473-482

    [14]

    ［14］Wei L. 2000. Two disequilibrium quartz-feldspar 18O/16O fractionations within the Aral granite batholith, Altay mountains of China: Evidence for occurrence of two stages of O and H isotopic exchange of a heterogeneous granite system with aqueous fluids. Journal of Petrology, 41(9): 1455-1466

    [15]

    ［15］Wu Yanchang. 1992. The magma skarn - a new kind of skarn. Anhui Geology, 2(1):12-26(in Chinese with English abstract)

    [16]

    ［16］Yasuhiro Kato. 1999. Rare earth elements as an indicator to origins of skarn deposits: examples of the Kamioka Zn-Pb and Yoshiwara-sannotake Cu(- Fe) deposits in Japan. Resource Geology, 49(4):183-198

    [17]

    ［17］Zeng Zhigang, Li Chaoyang, Liu Yuping and Tu Guangzhi. 1999. Geology and geochemistry of metamorphogenic skarn from Laojunshan metallogenic province. Acta Mineralogica Sinica, 19(1):48-45 (in Chinese with English abstrac)

    [18]

    ［18］Zhang Jian. 1998. Geology features of rare earth elements in veined skarn in Funiushan copper mine of Nanjing. Jiangsu Geology, 22(1): 15-18 (in Chinese with English abstract)

    [19]

    ［19］Zhao Yiming, Lin Wenwei, Bi Sicheng. 1990. Skarn deposits in China. Beijing: Geological Publishing House, 354 (in Chinese)

    [20]

    ［20］Zhao Yiming, Zhang Dequan and Others. 1997. Metallogeny and prospective evaluation of copper-polymetallic deposits in the Da Hinggan Mountains and its adjacent regions. Beijing: Seismological Press, 135-137 (in Chinese)

    [21]

    ［21］Zhao Zhenhua. 1997. Trace Elements Geochemistry. Beijing: Science Press, 1-153 (in Chinese)

    [22]

    陈骏, Halls C, Stanley C J. 1994. 柿竹园矽卡岩型钨锡钼矿床主要造岩矿物中REE的分布特征及成岩意义. 地球化学, 23(增刊):84-92

    [23]

    ［23］韩松, 黄忠祥,贾秀勤等. 1993. 云南个旧打磨山钙质矽卡岩及石榴石的稀土元素地球化学特征. 岩石学报, 9(2):192-197

    [24]

    ［24］李宏兵,王世杰,李朝阳,文锦明. 1997. 松潘-甘孜造山带中巴西金矽卡岩矿床成矿热液系统演化的(REE、Sr、O)证据. 矿物学报, 17(4):412-421

    [25]

    ［25］毛景文. 1987. 桂北BT锡矿稀土元素特征及其与成矿的关系. 河北地质学院学报,10(3):273-287

    [26]

    ［26］凌其聪,周贵斌,黄许陈, 颜玉琴. 1998. "层控式"矽卡岩矿床特征及成矿机制-以铜陵大团山铜(金)矿床为例. 贵金属地质, 7(2):91-95

    [27]

    ［27］潘家永,张乾,李朝阳. 2000. 滇西羊拉铜矿床稀土元素地球化学研究. 矿物学报, 20(1):44-49

    [28]

    ［28］邱瑞龙. 1987. 贵池铜山铜矿矽卡岩稀土元素地球化学. 地质学报, 61(1):91-100

    [29]

    王国政. 1997. 内蒙古安乐锡铜矿床地质特征成因. 矿床地质, 16(3):260-271

    [30]

    ［30］吴言昌. 1992. 论岩浆矽卡岩-一种新类型矽卡岩. 安徽地质, 2(1):12-26

    [31]

    曾志刚,李朝阳,刘玉平,涂光帜. 1999. 老君山矿区变质成因矽卡岩的地质地球化学特征. 矿物学报, 19(1):48-55

    [32]

    赵斌,赵劲松,刘海臣. 1999. 长江中下游地区若干Cu(Au)、Cu Fe(Au)和Fe矿床中钙质矽卡岩的稀土元素地球化学. 地球化学, 28(2):113-125

    [33]

    ［33］赵一鸣,林文蔚,毕成思等. 1990. 中国矽卡岩矿床. 北京:地质出版社, 354

    [34]

    ［34］赵一鸣,张德全等. 1999. 大兴安岭及其邻区铜多金属矿床成矿规律与远景评价. 地震出版社. 135-137

    [35]

    ［35］赵振华. 1997. 微量元素地球化学. 科学出版社, 1-153,

    [36]

    ［36］张建. 1998. 南京伏牛山铜矿脉状矽卡岩稀土元素地球化学特征. 江苏地质, 22(1):15-18

    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
WeChat 点击查看大图
计量
  • 文章访问数:  8141
  • PDF下载数:  8085
  • 施引文献:  0
出版历程
修回日期:  2001-11-18
刊出日期:  2002-11-30

目录

    返回

    地址：北京9825信箱/北京朝阳区北土城西路19号邮编：100029

    电话：(010) 82998205/82998135/82998137 邮箱：ysxb@mail.iggcas.ac.cn

    版权所有 © 2009-2023 岩石学报 京ICP备05029136号-23

    本系统由 北京仁和汇智信息技术有限公司开发