中国地质调查局西安地质调查中心主办
高级检索

甘肃北山地区花牛山群变英安岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其地质意义

,  ,  ,  ,  , 

文章导航 > 西北地质 > 2018 > 51(1): 54-64

上一篇

下一篇

谢建强, 第鹏飞, 杨婧, 陈万峰, 魏海峰, 翟新伟. 甘肃北山地区花牛山群变英安岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其地质意义[J]. 西北地质, 2018, 51(1): 54-64.
引用本文: 谢建强, 第鹏飞, 杨婧, 陈万峰, 魏海峰, 翟新伟. 甘肃北山地区花牛山群变英安岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其地质意义[J]. 西北地质, 2018, 51(1): 54-64.
shu
XIE Jianqiang, DI Pengfei, YANG Jing, CHEN Wanfeng, WEI Haifeng, ZHAI Xinwei. LA-ICP-MS Zircon U-Pb Age, Geochemistry and Tectonic Implications of Metamorphic Dacite from Huaniushan Group in Beishan Area, Gansu, China[J]. Northwestern Geology, 2018, 51(1): 54-64.
Citation: XIE Jianqiang, DI Pengfei, YANG Jing, CHEN Wanfeng, WEI Haifeng, ZHAI Xinwei. LA-ICP-MS Zircon U-Pb Age, Geochemistry and Tectonic Implications of Metamorphic Dacite from Huaniushan Group in Beishan Area, Gansu, China[J]. Northwestern Geology, 2018, 51(1): 54-64.
shu

甘肃北山地区花牛山群变英安岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其地质意义

  • 1.

    甘肃省矿产资源储量评审中心, 甘肃 兰州 730000

  • 2.

    甘肃省矿产资源储量评审中心, 甘肃 兰州 730000;兰州大学地质科学与矿产资源学院, 甘肃省西部矿产资源重点实验室(兰州大学), 甘肃 兰州 730000

  • 3.

    兰州大学地质科学与矿产资源学院, 甘肃省西部矿产资源重点实验室(兰州大学), 甘肃 兰州 730000

  • 4.

    甘肃省地质调查院, 甘肃 兰州 730000

  • 基金项目: 中国地质调查局“甘肃北山营毛沱-玉石山地区铁铜金钨多金属矿整装勘查区关键基础地质研究”（12120114014501）、国家自然科学基金项目“峨眉山大火成岩省钒钛磁铁矿矿床成矿机制的流体组成制约”（41472070）和中央高校基本科研业务费专项资金“金川Ni-Cu硫化物矿床成矿过程的Mg同位素组成示踪”（lzujbky-2017-77）资助

LA-ICP-MS Zircon U-Pb Age, Geochemistry and Tectonic Implications of Metamorphic Dacite from Huaniushan Group in Beishan Area, Gansu, China

  • 1.

    Gansu Assessment Center of Mineral Resources Reserves, Lanzhou 730000, Gansu, China

  • 2.

    Gansu Assessment Center of Mineral Resources Reserves, Lanzhou 730000, Gansu, China;Key Laboratory of Mineral Resources in Western China(Gansu Province), School of Earth Sciences, Lanzhou University, Lanzhou 730000, Gansu, China

  • 3.

    Key Laboratory of Mineral Resources in Western China(Gansu Province), School of Earth Sciences, Lanzhou University, Lanzhou 730000, Gansu, China

  • 4.

    Geological Survey of Gansu Province, Lanzhou 730000, Gansu, China

    摘要
  • 采用锆石U-Pb方法在甘肃北山地区花牛山群中变英安岩中获得LA-ICP-MS U-Pb年龄为（454.7±0.87）Ma（MSWD=0.28），属晚奥陶世早期的产物，该年龄可为准确厘定花牛山群的沉积时代提供新的依据，从而将其修订为上奥陶统。同时岩石地球化学具高碱、高铝，富集Rb、Th、U、K、Pb，亏损Nb、Ta、Ti，无明显δEu异常，显示出明显的火山弧岩浆特征。结合区域地质资料表明，岩体形成于活动大陆边缘，其形成与俯冲流体交代或俯冲沉积物的加入有关，与花牛山铅锌矿的喷流（气）沉积型块状硫化物矿床形成环境不同，因此，认为花牛山群并非花牛山铅锌矿的赋矿层位。
    By using the zircon LA-ICP-MS U-Pb dating, the obtained ages of metamorphic dacite from Huaniushan Group are (454.7 ±0.87)Ma (MSWD=0.28), which belong to the early stage of Late Ordovician.This age can provide a new basis for accurately determining the depositional age of Hunshan Group, thus the age of Hunshan Group has been revised as Upper Ordovician.This metamorphic dacite have high alkali and high Al, obvious enrichment of Rb, Th, U, K, Pb, negative anomalies of Nb, Ta, Ti, no obvious δEu anomaly, showing the typical volcanic magma characteristics.According to the regional geological data, the metamorphic dacite is formed in the active continental margin,which is related to the addition of subduction fluid or subduction sediments and is different from the formation of massive sulfide deposits in the Huaniushan Pb-Zn deposit.Therefore, it is considered that the Huaniushan Group is not the ore-bearing strata of Huaniushan Pb-Zn deposit.
    • HTML全文
  • 加载中
    • 参考文献(30)

  • 代文军,龚全胜,李海林,等.甘肃北山南带中段志留系的发现及地质意义[J].西北地质,2002,35(3):42-47.

    DAI Wenjun,GONG Quansheng,LI Hailin,et al.Discovery of Silurian in middle section of south belt of Beishan mountain and its geological significance,Gansu[J].Northwestern Geology,2002,35(3):42-47.

    龚全胜,刘明强,李海林,等.甘肃北山造山带类型及基本特征[J].西北地质,2002,35(3):28-34.

    GONG Quansheng,LIU Mingqiang,LI Hailin,et al.The type and basic characteristics of Beishan orogenic belt,Gansu[J].Northwestern Geology,2002,35(3):28-34.

    何世平,任秉琛,姚文光,等.甘肃内蒙古北山地区构造单元划分[J].西北地质,2002,35(4):30-40.

    HE Shiping,REN Binchen,YAO Wenguang,et al.The division of tectonic units of Beishan area, Gansu-Inner Mongolia[J].Northwestern Geology,2002,35(4):30-40.

    贺振宇,宗克清,姜洪颖,等.北山造山带南部早古生代构造演化:来自花岗岩的约束[J].岩石学报,2014,30(8):2324-2338.

    HE Zhenyu,ZONG Keqing,JIANG Hongyin,et al.Early Paleozoic tectonic evolution of the southern Beishan orogenic collage:Insights from the granitoids[J].Acta Petrologica Sinica,2014,30(8):2324-2338.

    刘雪亚,王荃.中国西部北山造山带的大地构造及其演化[A].中国地质科学院地质研究所文集[C],1995,37-48.

    LIU Xueya,WANG Quan.Tectonics of orogenic belts in beishan mts.,western china and their evolution[A].CAGS[C[,1995,37-48.

    聂凤军,江思宏,刘妍,等.甘肃花牛山东钾长花岗岩40Ar/39Ar同位素年龄及其地质意义[J].地质科学,2002b,37(4):415-422.

    NIE Fengjun,JIANG Sihong,LIU Yan,et al.40Ar/39Ar isotopic age dating on k-feldspar separates from eastern Haniushan granite, Gnsu province, and its geological significance[J].Scientia Geologica Sinica,2002b,37(4):415-422.

    聂凤军,江恩宏,白天明,等.北山地区金属矿床成矿规律及找矿方向[M].北京:地质出版社,2002a.

    NIE Fengjun,JIANF Sihong,BAI Tianming,et al.Metallogenic studies and ore prospecting in the conjunction area of Inner Mongolia Autonomous Region, Gansu Province and Xinjiang Uygur Autonomous Region (Beishan Mt.),Northwest China[M].Beijing:Geological Publishing House,2002a.

    杨合群,李英,赵国斌,等.北山蛇绿岩特征及构造属性[J].西北地质,2010,43(1):26-36.

    YANG Hequn,LI Ying,ZHAO Guobin,et al.Character and structural attribute of the Beishan ophiolite[J].Northwestern Geology,2010,43(1):26-36.

    杨建国,翟金元,杨宏武,等.甘肃北山地区花牛山铅锌矿区玄武岩锆石LA-ICP-MS U-Pb定年及其地质意义[J].地质通报,2010,29(7):1017-1023.

    YANG Jianguo,ZHAI Jinyuan,YANG Hongwu,et al.LA-ICP-MS zircon U-Pb dating of basalt and its geological significance in Huaniushan Pb-Zn deposit,Beishan area,Gansu,China[J].Geological Bulletin of China,2010,29(7):1017-1023.

    杨建国.甘肃北山花牛山金银多金属矿田成矿规律与找矿预测[M].北京:地质出版社,2011.

    YANG Jianguo.Metallogenic studies and ore prospecting in Huaniushan gold and silver polymetallic ore field,Beishan,Gansu,China[M].Beijing:Geological Publishing House,2011.

    殷勇,殷先明.花牛山地区中生代A型花岗岩特征及其找矿意义[J].甘肃地质,2010,19(1):6-14.

    YIN Yong,YIN Xianming.Features of mesozoic A-type granites and it's significancesfor prospecting in Huaniushan area[J].Gansu Geology,2010,19(1):6-14.

    余吉远,王国强,李向民,等.北山地区花牛山群的重新厘定——来自火山岩地球化学证据[J].新疆地质,2015,33(4):537-543.

    YU Jiyuan,WANG Guoqiang,LI Xiangmin,et al.The redefinition of Huaniushan Group in Beishan area:geochemical evidence from volcanic rocks[J].Xinjiang Geology,2015,33(4):537-543.

    张铭杰,吴茂炳.花牛山铅锌矿床成因的矿物学—?桛畊湝洮椘溃朰?攬琱?愹永?倷爨漲瘩攺渹愳渭挹攸?漼晢?派敚瑈慁獎敇搠楍浩敮湧瑪慩牥礬?牕漠捍歡獯?晩牮潧洮?琠桭敩??敲楡獬桯慧湩?潡牬漠杳整湵楤捹?捯潮氠汴慨来攠?獥潮略瑳桩敳爠湯??汈瑵慡楮摩獵?捨潡湮猠瑬牥慡楤渭瑺獩?晣爠潤浥?摯敳瑩牴楛瑊慝氮?穡楮牳捵漠湇?啯?偯执?愬渱搹??昬?椨猲漩琺漹瀳椭挹?搮愼瑢慲嬾?巽??濭滬摰眬憋滅愮‘劃攗獱旳懭爰挺梱?医ほ??拣?????????五????????拳牦?听??丰?娬栲漳渨朸栩町愱?場??伱?圶攰渮樼楢慲漾?坈?乏???奨?????敏琠?慨污?卪瑩牥甬捗瑁畎片攠?慩朮敇?慯湣摨?瑯敮捯瑬潯湧楹挬?摥敯癣敨汥潭灩浣敡湬琠?潨晡?瑡档整??畩潳獴桩楣獳栠慡湮?丠楴略橣畴慯湮穩楣?潩灭桰楬潩汣楡瑴楩捯?浳??????汥愠湧杲敡??整楯獩桤慳渠?獲潯畭琠桌敩牵湹浵潡獮琠??汥瑡愬楂摥獩孳?嵡??潇湡摮睳慵渠慰?副敶獩敮慣牥挬桎??ぴ??????至????せ??????扡爠?坥?乲???卧呩?剡???????伬夲?‰倷????攸漩挺栱攸洴椷挭愱永?洰愮朼浢慲￣琱祟瀮攗?搠楱猦捗爦榄洠椭溩慆瓺椠漎滑?懑灞瀐泿楛捄慝琮椭濽渰?琧潦?愲氰琱攳爮攼摢?愾湚摈?洠敊瑩慡浮潧爮灔桥潣獴敯摮?戭慭獡楧捭?楴杩湣攠潦畯獲?牡潴捩歯獮嬠?嵮??慧牯瑬桤???偬汹愠湭敥瑴慡牬祬?卣挠業敩湮捥敲??敩瑺瑡整物獯?ㄠ???????????????????扥牡?坎?丠???奮????????塮???噮???塲楳慩潴?圠敯湦樠楇慥潯?散瑩?慮汣?味攬挲琰漱渳椮挼?浲漾擦旽氝猬?曽漦爬?憢揚挮爗敱瑿楗澄渠?漐替?璋桛敍??攗溬琺爗憬氧??獈椾愬渱?伹爰潡朮攼湢楲挾??敏氠瑇孵?嵣??潯甬版湅愠汇?潯晱?琬桌敉??敯潮汧潣杨楥据慧氮?卬潡捴楥攠瑴祥??はの????????????????扯牧?塮??传?坥敧湵橬楡慴潩?坳?乩???奥?????????剩?????攮瑂?慩汪?偮慧氺慐敥潫穩潮楧挠?慮捩捶牥敲瑳楩潴湹愠牐祵?慬湩摣?捴潩湯癮攬爱朹改渰瑡?琼敢捲琾濦滽椝挬猘?濑昬‘琥棕攮‘现澙甗瑱栰攺犄渠??泊琔愖楛摊獝?椘涃瀰氨椬挲愰琰椳漬渱猲?昱漩爺?琭栱攵?朼牢潲眾瑚桕?漠晇??散湨瑡牯愬汌??猠楙慩孫?崬??潕甠牃湨慵汮?潡普?瑆桲敡??敷潯汲潫朠楡据慤氠?卶潯捬極整瑩祯?㈠はて?慴?????????????????扴牵?塥??佮?坢敥湩橳楨慡潮?婡??乡???楲慯湳捳栠慧湡杮?兵?买??敶穩桮慣湥本?數瑩?慪汩?偮慧氠敡潵穴潯楮捯?慯捵捳爠敲瑥楧潩湯慮爠祡?慤渠摉?据潥汲氠楍獯楮潧湯慬汩?琠敡捵瑴潯湮楯捭獯?潳映?瑥桧敩??慛獊瑝攮片湡?味極愠湇獥桯慬湯???栲椰渰愳??椲洨瀱氩椺挱愭琱椵漮渼獢?显濦狽”琬栠旑?挬潕滽琦椬湉攮渗瑱愰氺?柤爟濣睿瑗梄?潹暁?捊敝渮琰爨懑汦??猹椹愰孢?崴??洰攵爭椳挱愴渮??潲甾牚湕慏氠?潵景?卨捡楯攬湚捈敁???こ?扵??の???????は????? al.Early Paleozoic plate tectonics in Beishan Area[J].Chinese Journal of Geology,1990b,4:305-314.

    CONDIE K C.Geochemical changes in baslts and andesites across the Archean-Proterozoic boundary:Identification and significance[J].Lithos,1989,23(1):1-18.

    HOSKIN P W O,SCHALTEGGER U.The composition of zircon and igneous and metamorphic petrogenesis[J].Reviews in mineralogy and geochemistry,2003,53(1):27-62.

    JAHN B,WINDLEY B,NATAL'IN B,et al.Phanerozoic continental growth in Central Asia[J].Journal of Asian Earth Sciences,2004,23(5):599-603.

    SONG Dongfang,XIAO Wenjiao,HAN Chunming,et al.Progressive accretionary tectonics of the Beishan orogenic collage,southern Altaids:insights from zircon U-Pb and Hf isotopic data of high-grade complexes[J].Precambrian Research,2013a,227:368-388.

    SONG Dongfang,XIAO Wenjiao,HAN

    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
计量
  • 文章访问数:  2552
  • PDF下载数:  2005
  • 施引文献:  0
出版历程
收稿日期:  2017-08-13
修回日期:  2017-11-25
刊出日期:  2018-03-15

目录

    版权所有：中国地质调查局发展研究中心 copyright @2020
    返回