Xi'an Center, China Geological SurveyHost
Advanced Search
Previous Article Next Article
2019 Vol. 52, No. 4
Article Contents
Article navigation > Northwestern Geology > 2019 > 52(4): 137-151
Next Article Previous Article

ZHANG Qiang, FENG Changrong, XIE Yueqiao, WANG Haijun, HAO Yanhai. 2019. Geochemical Characteristics and Genetic Study of Mokaer Magnetite Deposits in the Taxkorgan Area, Xinjiang. Northwestern Geology, 52(4): 137-151.
Citation: ZHANG Qiang, FENG Changrong, XIE Yueqiao, WANG Haijun, HAO Yanhai. 2019. Geochemical Characteristics and Genetic Study of Mokaer Magnetite Deposits in the Taxkorgan Area, Xinjiang. Northwestern Geology, 52(4): 137-151.
shu

Geochemical Characteristics and Genetic Study of Mokaer Magnetite Deposits in the Taxkorgan Area, Xinjiang

  • No.2 Geological Party, Xinjiang Bureau of Geology and Mineral Resource Exploration, Kashi 844002, Xinjiang, China

Received Date:  10 August 2019
Revised Date:  01 September 2019
    Abstract
  • Mokaer magnetite deposit is located in Maeryang Township, Taxkorgan County, Xinjiang. Thereare11 magnetite belts(940~3 800m long and 2~150m thick) and 4 magnetite mineralization belts(150~240m long and 2~12m thick) have been found in the deposit. The ore bodies occur in the Proterozoic Bulunkuole Group, and the ore bodies are in gradual contact with the surrounding rocks. The ore bodies are mostly controlled by plagioclase amphibolite, biotite plagioclase gneiss and biotite quartz schist. The rare earth elements in ores in this deposit are generally of right-leaning type and enriched with light rare earth elements, with weak positive Ce anomalies, enriched with U, La, Pb, Pr, Sm, Nd, and depleted with Ta, Sr, Ti, Zr and Hf. The Fecontent of magnetite is 99.08% to 99.64%, with an average of 99.35%. Geochemical characteristics of wall rocks, ores and magnetite show that the deposit has the characteristics of sedimentary metamorphic iron ores, and that the deposit has been subjected to later hydrothermal reformation and mixed with a considerable proportion of terrigenous clastic materials.
    • FullText(HTML)
  • 加载中
    • References
  • 河南省地质调查院.新疆塔什库尔干-莎车铁铅锌多金属矿评价报告[R].2009.

    Google Scholar

    杨国林,何雨栗,王文佳,等.新疆塔什库尔干吉尔铁克铁矿地质特征及成因[J].兰州大学学报(自然科学版),2015,51(04):462-469+477.

    Google Scholar

    YANG Guolin, HE Yuli,WANG Wenjia,et al. Geological characteristics and genesis of Jiertieke iron deposit in Taxkorgan Area, Xinjiang Province[J]. Journal of Lanzhou University (Natural Sciences), 2015,51(04):462-469+477.

    Google Scholar

    乔耿彪,王萍,伍跃中,等.西昆仑塔什库尔干陆块赞坎铁矿赋矿地层形成时代及其地质意义[J].中国地质,2015,42(03):616-629.

    Google Scholar

    QIAO Gengbiao, WANG Ping, WU Yuezhong, et al. Formation age of ore-bearing strata of the Zankan iron deposit in Taxkorgan landmass of Western Kunlun Mountains and its geological significance[J].Geology in China, 2015, 42(3):616-629.

    Google Scholar

    刘品德.西昆仑塔什库尔干地区老并石膏磁铁矿地质特征及成矿作用过程探讨[J].西北地质,2014,47(04):227-236.

    Google Scholar

    LIU Pinde. Geological Features and Mineralization Process of Laobing Gypsum Magnetite Deposit in Taxkorgan Region of West Kunlun[J].Northwestern Geology, 2014,47(04):227-236.

    Google Scholar

    钱兵,高永宝,李侃,等.塔什库尔干地区赞坎铁矿矿物学特征与成因[J].地质与勘探,2014,50(04):630-640.

    Google Scholar

    QIAN Bing, GAO Yongbao, LI Kan, et al. Mineralogy and genesis of the Zankan iron deposit in Taxkorgan area, Xinjiang[J].Geology and Exploration, 2014, 50(4):630 -640.

    Google Scholar

    丁明朋,汤好书,陈衍景,等.西昆仑塔什库尔干叶里克铁矿成因:矿床地质与磁铁矿LA-ICP-MS原位分析约束[J].地球科学,2018,43(09):3169-3185.

    Google Scholar

    DING Mingpeng,TANG Haoshu,CHEN Yanjing,et al.Genesis of the Erik Iron Ore Deposit in the Taxkorgan Area of the West Kunlun,Xinjiang:Constraints from Ore Deposit Geology and In Situ LA-ICP-MS Analysis of Magnetite[J].Earth Science, 2018,43(09):3169-3185.

    Google Scholar

    陈俊魁.新疆西昆仑塔什库尔干地区老并铁矿赋矿地层形成时代及其地质意义[J].西北地质,2018,51(03):105-120.

    Google Scholar

    CHEN Junkui. Formation Age of Ore-bearing Strata from the Laobing Iron Deposit in Taxkorgan area of Western Kunlun,Xinjiang and Its Geological Significance[J]. Northwestern Geology, 2018,51(03):105-120.

    Google Scholar

    陈登辉,伍跃中,李文明,等. 西昆仑塔什库尔干地区磁铁矿矿床特征及其成因[J]. 大地构造与成矿学, 2013,37(4):671-684.

    Google Scholar

    CHEN Denghui, WU Yuezhong, LI Wenming, et al. Geological Characteristics and Genesis of the Iron Deposits in the Taxkorgan Area, West Kunlun[J]. Geotectonica et Metallogenia, 2013,37(4):671-684.

    Google Scholar

    李智泉,张连昌,薛春纪,等.西昆仑赞坎铁矿床地质特征、形成时代及高品位矿石的成因[J].岩石学报,2018,34(02):427-446.

    Google Scholar

    LI Zhiquan, ZHANG Lianchang, XIE Chunji, et al.Geological characteristics,formation age and high-grade ore genesis of Zankan banded iron deposit in the West Kunlun Mountains[J]. Acta Petrologica Sinica,2018,34(02):427-446.

    Google Scholar

    张强.新疆塔什库尔干县莫喀尔磁铁矿床成矿地质特征与找矿方向[D].中国地质大学(武汉),2016.

    Google Scholar

    ZHANG Qiang. Geological characteristics and prospecting direction of the mokaer Fe deposit in Tashikuergan county, Xinjiang[D].China University of Geosciences(Wuhan), 2016.

    Google Scholar

    沈其韩,宋会侠,杨崇辉,等.山西五台山和冀东迁安地区条带状铁矿的岩石化学特征及其地质意义[J].岩石矿物学杂志, 2011,30(2):161-171.

    Google Scholar

    SHEN Qihank, SONG Huixia, YANG Chonghuil, et al. Petrochemical characteristics and geological significations of banded iron formations in the Wutai Mountain of Shanxi and Qian an of eastern Hebei[J].Acta Petrologica et Mineralogica, 2011,30(2):161-171.

    Google Scholar

    计文化,李荣社,陈守建,等.甜水海地块古元古代火山岩的发现及其地质意义[J].中国科学:地球科学, 2011,41(9):1268-1280.

    Google Scholar

    JI Wenhua, LI Rongshe, CHEN Shoujian, et al. The discovery of Palaeoproterozoic volcanic rocks in the Bulunkuoler Group from the Tianshuihaimassif in Xinjiang of Northwest china and its geological significance[J]..Sci China Earth Sci, 2011,41(9):1268-1280.

    Google Scholar

    李志红, 朱祥坤, 唐索寒. 鞍山-本溪地区条带状铁建造的铁同位素与稀土元素特征及其对成矿物质来源的指示[J]. 岩石矿物学杂志, 2008, 27(4):285-290.

    Google Scholar

    LI Zhihong, ZHU Xiangkun, TANG Suohan. Characters of Fe isotopes and rare earth elements of banded iron formations from Anshan-Benxi area:implications for Fe source[J]. Acta Petrologica et Mineralogica, 2008, 27(4):285-290.

    Google Scholar

    闫斌, 朱祥坤, 唐索寒,等. 广西新元古代BIF的铁同位素特征及其地质意义[J]. 地质学报, 2010, 84(7):1080-1086.

    Google Scholar

    YAN Bin, ZHU Xiangkun, TANG Suohan, et al.Fe Isotopic Characteristics of the Neoproterozoic BIF in Guangxi Province and its Implications[J].Acta Geologica Sinica, 2010, 84(7):1080-1086.

    Google Scholar

    丁文君, 陈正乐, 陈柏林, 等. 河北迁安杏山铁矿床地球化学特征及其对成矿物质来源的指示[J]. 地质力学学报, 2009, 15(4):363-373.

    Google Scholar

    DING Wenjun, CHEN Zhengle, CHEN Bolin,et al. Geological characters of band iron formation from Xinshan iron deposit in QianAn area, Hebei province:implication for their origin[J].Hournal of Geomechanics, 2009, 15(4):363-373.

    Google Scholar

    王守伦, 刘其严, 张殿学, 等. 闽粤地区海底热液喷气成因铁矿床的地球化学特征[J]. 地质找矿论丛, 1993, (3):14-27.

    Google Scholar

    WANG Shoulun, LIU Yanxue, ZHANG Dianxue, et al. Geochemical characteristics of sub-marine hydrothermal exhalated Fe-deposits in Fujian-Guangdong area[J]. Contributions To Geology and Mineral Resources Research,1993, (3):14-27.

    Google Scholar

    杜后发,姜勇彪, 侯增谦,等. 囊谦古近纪盆地砂岩地球化学特征及其对物源和沉积环境的指示作用. 岩石矿物学杂志, 2011,30(4):654-664.

    Google Scholar

    DU Houfa, JIANG Yongbiao, HOU Zengqian, et al. Geochemical characteristics of Paleogene sandstones in Nangqen basin and their implications for provenance and sedimentary environments[J]. Actapetrologica et Mineralogica,2011,30(4):654-664.

    Google Scholar

    姚纪明, 于炳松, 陈建强,等. 中扬子北缘上侏罗统-白垩系沉积岩地球化学特征与构造背景分析[J]. 地球化学, 2009, 38(3):231-241.

    Google Scholar

    YAO Jiming, YU Bingsong, CHEN Jianqiang, et al. The geochemical characteristics of the Upper Jurassic to Cretaceous sedimentary rocks in north margin of the mid-Yangtze and tectonic setting discrimination[J].Geochimica, 2009, 38(3):231-241.

    Google Scholar

    陈述荣, 谢家亨, 许超南,等. 福建龙岩马坑铁矿床成因的探讨[J]. 地球化学, 1985(4):350-357.

    Google Scholar

    CHEN Shurong, XIE Jiaheng, XU Chaonan, et al. The origin of making iron deposit, Fujian[J]. Geochimica, 1985(4):350-357.

    Google Scholar

    张连昌,翟明国,万渝生等.华北克拉通前寒武BIF铁矿研究:进展与问题[J]. 岩石学报, 2012,28 (11):3431-3445.

    Google Scholar

    ZHANG Lianchang, ZHAI Mingguo, WAN Yusheng, et al. Study of the Precambrian BIF-iron deposits in the North China Craton:Progresses and questions[J]. Acta Petrologica Sinica, 2012,28(11):3431-3445.

    Google Scholar

    徐国风, 邵洁涟. 磁铁矿的标型特征及其实际意义[J]. 地质与勘探, 1979, 26(3):541-546.

    Google Scholar

    XU Guofeng, SHAO Jielian. Typomorphic characteristics of magnetite and its practical significance[J].Geology and Prospecting, 1979, 26(3):541-546.

    Google Scholar

    陈光远, 黎美华, 汪雪芳, 等. 弓长岭铁矿成因矿物学专辑第二章磁铁矿[J]. 矿物岩石, 1984(2):20-47.

    Google Scholar

    林师整.磁铁矿矿物化学、成因及演化的探讨[J].矿物学报,1982, 2(3):166-174.

    Google Scholar

    LIN Shizheng. A contribution to the chemistry, origin and evolution of magnetite[J].Acta Mineralogica Sinica, 1982, 2(3):166-174.

    Google Scholar

    宋樾. 塔什库尔干地区铁矿成因类型及成矿环境研究[D]. 吉林大学, 2019.

    Google Scholar

    SONG Yue. Study on Genetic Types and Metallogenic Environment of Iron Deposits in the Taxkorgan Area[D]. Ji lin University, 2019.

    Google Scholar

    SUN SS, MCDonough WF. Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 1989, 42:313-345.

    Google Scholar

    BHATIA MR, Taylor SR. Trace-element geochemistry and sedimentary provinces:A study from the Tasman Geosyncline, Australia[J]. Chemical Geology,1981, 33(1-4):115-125.

    Google Scholar

    ANNERSTEN H.A mineral chemical study of a metamorphosed iron formation in northern Sweden[J].Lithos,1968,1(4):374-397

    Google Scholar

    RUMBLE D III.Fe-Ti oxide minerals from regionally metamorphosed quartzites of western New Hampshire[J].Contributions to Mineralogy and Petrology,1973,42 (3):181 -195.

    Google Scholar

    DUPUIS C, Beaudoin G. Discriminant diagrams for iron oxide trace element fingerprinting of mineral deposit types[J]. Mineralium Deposita, 2011, 46 (4):319-335.

    Google Scholar

    SUGITANI K. Geochemical characteristic of Archean cherts and other sedimentary rocks in the Pilbara Block, Western Australia:Evidence for the Archean sea-water enrichedin hydrothermally-derived iron and silica[J].Precambrian Research, 1992, 57(1-2):21-47.

    Google Scholar

    DANIELSON A, MÖLLER P, DULSKI P. The europium anomalies in banded iron formations and the thermal history of the oceanic crust[J]. Chemical Geology, 1992,97(1-2):89-100.

    Google Scholar

    BAU M, DULSKI P. Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron formations, Transvaal Supergroup, South Africa[J]. Precambrian Research, 1996,79(1):37-55.

    Google Scholar

    DOUVILLE E, BIENVENU P, CHARLOU JL. Yttrium and rare earth elements in fluids from various deep-sea hydrothermal systems[J]. Geochimica et Cosmochimica Acta, 1999,63(5):627-643.

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索
Export Citation
PDF
XML

Article Metrics

Article views(1175) PDF downloads(782) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020