大兴安岭南段维拉斯托锡多金属矿床LA-ICP-MS锡石和锆石U-Pb年龄及其地质意义
|
摘要
维拉斯托锡多金属矿床位于大兴安岭南段西坡的内蒙古克什克腾旗,是近年来发现的一个以锡为主,共伴生钨、锌、铜、钼、铷、铌和钽的大型矿床。矿化类型包括深部以锡为主,伴生锌、铷、铌和钽的蚀变花岗岩型矿体;中部以锡为主,伴生铜和锌的隐爆角砾岩型矿体及浅部锡、钨、锌、铜和钼的石英大脉型和网脉型矿体。该矿床的主要工业矿体为石英脉型,呈北北东向产于古元古界宝音图群和华力西期石英闪长岩中的断裂破碎带内,而蚀变花岗岩型和隐爆角砾岩型矿石的品位较低。文中选取1件石英脉型锡矿体中的锡石样品进行了LA-ICP-MS锡石U-Pb定年,获得锡石的~(206)Pb/~(207)Pb~(238)U/~(207)Pb等时线年龄为(136.0±6.1)Ma(MSWD=0.94),~(207)Pb/~(206)Pb-~(238)U/~206)Pb谐和年龄为(132.3±5.4)Ma(MSWD=2.8),表明维拉斯托锡多金属矿床形成于早白垩世;选取1件与成矿相关的北大山岩体花岗岩样品开展了LA-ICP-MS锆石U-Pb定年,获得~(206)Pb/~(238) U年龄为(140±2)Ma(MSWD=0.10),表明成矿岩体亦形成于早白垩世。维拉斯托锡多金属矿床属于与花岗岩有关的岩浆-热液型矿床。通过统计大兴安岭南段主要锡多金属矿床的成矿年龄和成矿岩体的年龄,发现几乎所有的锡多金属矿床均形成于140~135Ma期间,表明早白垩世是大兴安岭南段锡多金属矿床成矿高峰期。
The Weilasituo tin-polymetallic deposit,located in Hexigten Banner of Inner Mongolia,is a newly discovered large tin deposit associated with tungsten,zinc,copper,molybdenum,rubidium,niobium and tantalum the west slope of the southern Great Xing'an Range.Three types of mineralization developed in the deposit:the deep section altered granite-type orebody is dominated by Sn and associated with Zn,Rb,Nb;the middle section cryptoexplosive breccia-type orebody is mainly of Sn with Cu and Zn;and the shallow section comprises quartz vein-type Sn,W,Zn,Cu,and Mo ore bodies.The quartz vein-type ore bodies are the most economically valuable ores,they are hosted within the NNE-trending shattered fault zones of the Paleoproterozoic Baoyintu Group and Middle Variscan quartz diorite,whereas the altered granite-and cryptoexplosive breccia-type ore bodies are usually low grade ores.A cassiterite sample from the quartz vein-type Sn ore of the Weilasituo deposit was selected for LA-ICP-MS dating,which yielded a206 Pb/207 Pb-238 U/207 Pb isochron age of 136.0±6.1 Ma(MSWD=0.94)and a 207 Pb/206 Pb-238 U/206 Pb concordant age of 132.3±5.4 Ma(MSWD=2.8).The result suggested that the Weilasituo Sn-polymetallic mineralization took place during the Early Cretaceous.A zircon sample from the Beidashan granite was also selected for LA-ICP-MS dating,and the result of a weighted mean 206 Pb/238 U age of 140±2 Ma(MSWD=0.10)indicated the ore causative intrusion also formed during the Early Cretaceous.The Weilasituo tinpolymetallic deposit belongs to a granite-related magmatic-hydrothermal deposit.Our dating results,together with previous researchers' rock-and ore-forming ages of other Sn-polymetallic deposits in the southern Great Xing'an Range,demonstrated that almost all Sn-polymetallic deposits formed during 140-135 Ma,which suggests that the Early Cretaceous is the peak era for the formation of the Sn-polymetallic deposits in the southern Great Xing'an Range.
The Weilasituo tin-polymetallic deposit,located in Hexigten Banner of Inner Mongolia,is a newly discovered large tin deposit associated with tungsten,zinc,copper,molybdenum,rubidium,niobium and tantalum the west slope of the southern Great Xing'an Range.Three types of mineralization developed in the deposit:the deep section altered granite-type orebody is dominated by Sn and associated with Zn,Rb,Nb;the middle section cryptoexplosive breccia-type orebody is mainly of Sn with Cu and Zn;and the shallow section comprises quartz vein-type Sn,W,Zn,Cu,and Mo ore bodies.The quartz vein-type ore bodies are the most economically valuable ores,they are hosted within the NNE-trending shattered fault zones of the Paleoproterozoic Baoyintu Group and Middle Variscan quartz diorite,whereas the altered granite-and cryptoexplosive breccia-type ore bodies are usually low grade ores.A cassiterite sample from the quartz vein-type Sn ore of the Weilasituo deposit was selected for LA-ICP-MS dating,which yielded a206 Pb/207 Pb-238 U/207 Pb isochron age of 136.0±6.1 Ma(MSWD=0.94)and a 207 Pb/206 Pb-238 U/206 Pb concordant age of 132.3±5.4 Ma(MSWD=2.8).The result suggested that the Weilasituo Sn-polymetallic mineralization took place during the Early Cretaceous.A zircon sample from the Beidashan granite was also selected for LA-ICP-MS dating,and the result of a weighted mean 206 Pb/238 U age of 140±2 Ma(MSWD=0.10)indicated the ore causative intrusion also formed during the Early Cretaceous.The Weilasituo tinpolymetallic deposit belongs to a granite-related magmatic-hydrothermal deposit.Our dating results,together with previous researchers' rock-and ore-forming ages of other Sn-polymetallic deposits in the southern Great Xing'an Range,demonstrated that almost all Sn-polymetallic deposits formed during 140-135 Ma,which suggests that the Early Cretaceous is the peak era for the formation of the Sn-polymetallic deposits in the southern Great Xing'an Range.
引文
[1]徐志刚,陈毓川,王登红,等.中国成矿区带划分方案[M].北京:地质出版社,2008:1-138.
[2]赵一鸣,张德全.大兴安岭及其邻区铜多金属矿床成矿规律与远景评价[M].北京:地震出版社,1997:1-318.
[3]毛景文,周振华,武广,等.内蒙古及邻区矿床成矿规律与成矿系列[J].矿床地质,2013,32(4):716-730.
[4]陈郑辉,王登红,盛继福,等.中国锡矿成矿规律概要[J].地质学报,2015,89(6):1026-1037.
[5]OUYANG H G,MAO J W,ZHOU Z H,et al.Late Mesozoic metallogeny and intracontinental magmatism,southern Great Xing’an Range,northeastern China[J].Gondwana Research,2015,27(3):1153-1172.
[6]王春女,王全明,于晓飞,等.大兴安岭南段锡矿成矿特征及找矿前景[J].地质与勘探,2016,52(2):220-227.
[7]ZHOU Z H,MAO J W,LYCKBERG P,et al.Geochronology and isotopic geochemistry of the A-type granites from the Huanggang Sn-Fe deposit,southern Great Hinggan Range,NE China:implication for their origin and tectonic setting[J].Journal of Asian Earth Sciences,2012,49(3):272-286.
[8]LIU Y F,JIANG S H,BAGAS L.The genesis of metal zonation in the Weilasituo and Bairendaba Ag-Zn-Pb-Cu-(SnW)deposits in the shallow part of a porphyry Sn-W-Rb system,Inner Mongolia,China[J].Ore Geology Reviews,2016,75(2):150-173.
[9]WANG F X,BAGAS L,JIANG S H,et al.Geological,geochemical,and geochronological characteristics of Weilasituo Sn-polymetal deposit,Inner Mongolia,China[J].Ore Geology Reviews,2017,80:1206-1229.
[10]江思宏,聂凤军,刘翼飞,等.内蒙古拜仁达坝及维拉斯托银多金属矿床的硫和铅同位素研究[J].矿床地质,2010,28(1):101-112.
[11]OUYANG H G,MAO J W,SANTOSH M,et al.The early Cretaceous Weilasituo Zn-Cu-Ag vein deposit in the southern Great Xing’an Range,northeast China:fluid inclusions,H,O,S,Pb isotope geochemistry and genetic implications[J].Ore Geology Reviews,2014,56:503-515.
[12]内蒙古维拉斯托矿业有限责任公司,内蒙古地质勘查有限责任公司.内蒙古自治区克什克腾旗维拉斯托矿区锡多金属矿勘探报告[R].呼和浩特:内蒙古自治区地质调查院,2015:1-112.
[13]王瑾,侯青叶,陈岳龙,等.内蒙古维拉斯托铜多金属矿床流体包裹体研究[J].现代地质,2010,24(5):847-855.
[14]申伍军,王学求,聂兰仕.大兴安岭成矿带大型银多金属矿区域地球化学预测指标[J].地学前缘,2012,19(3):49-58.
[15]刘翼飞,聂凤军,江思宏,等.内蒙古拜仁达坝铅-锌-银矿床:元素分带及其成因[J].吉林大学学报(地球科学版),2012,42(4):1055-1068.
[16]刘翼飞,樊志勇,蒋胡灿,等.内蒙古维拉斯托-拜仁达坝斑岩-热液脉状成矿体系研究[J].地质学报,2014,88(12):2373-2385.
[17]欧阳荷根.大兴安岭南段拜仁达坝-维拉斯托银多金属矿床成矿作用及动力学背景[D].北京:中国地质大学(北京),2013:1-192.
[18]梅微,吕新彪,唐然坤,等.大兴安岭南段西坡拜仁达坝-维拉斯托矿床成矿流体特征及其演化[J].地球科学:中国地质大学学报,2015,40(1):145-162.
[19]潘小菲,郭利军,王硕,等.内蒙古维拉斯托铜锌矿床的白云母Ar/Ar年龄探讨[J].岩石矿物学杂志,2009,28(5):473-479.
[20]翟德高,刘家军,李俊明,等.内蒙古维拉斯托斑岩型锡矿床成岩、成矿时代及其地质意义[J].矿床地质,2016,35(5):1011-1022.
[21]郭贵娟.内蒙古维拉斯托锡多金属矿床地质特征及成因探讨[D].北京:中国地质大学(北京),2016:1-70.
[22]祝新友,张志辉,付旭,等.内蒙古赤峰维拉斯托大型锡多金属矿的地质地球化学特征[J].中国地质,2016,43(1):188-208.
[23]王瑾.内蒙古维拉斯托铜多金属矿床矿区花岗岩类年代学与地球化学[D].北京:中国地质大学(北京),2009:1-68.
[24]王新宇,侯青叶,王瑾,等.内蒙古维拉斯托矿床花岗岩类SHRIMP年代学及Hf同位素研究[J].现代地质,2013,27(1):67-78.
[25]薛怀民,郭利军,侯增谦,等.大兴安岭西南坡成矿带晚古生代中期未变质岩浆岩的SHRIMP锆石U-Pb年代学[J].岩石矿物学杂志,2010,29(6):811-823.
[26]刘翼飞.内蒙古克什克腾旗拜仁达坝银多金属矿床成因研究[D].北京:中国地质科学院,2009:1-98.
[27]樊志勇,邱慧远,付旭,等.内蒙古维拉斯托大型斑岩型锡多金属找矿勘查及启示[J].黄金科技技术,2017,25(1):9-17.
[28]YUAN S D,PENG J T,HU R Z,et al.In-situ LA-MC-ICP-MS and ID-TIMS U-Pb geochronology of cassiterite in the giant Furong tin deposit,Hunan Province,South China:new constraints on the timing of tin-polymetallic mineralization[J].Ore Geology Reviews,2011,43(1):235-242.
[29]ANDERSEN T.Correction of common lead in U-Pb analyses that do not report 204Pb[J].Chemical Geology,2002,192(1):59-79.
[30]LUDWIG K R.Isoplot:aplotting and regression program for radiogenic-isotope data[R].USGS Open-File Report,1997,Version 2.92:91-445.
[31]GRIFFIN W L,BELOUSOVA E A,SHEE S R,et al.Archean crustal evolution in the northern Yilgarn Craton:U-Pb and Hf-isotope evidence from detrital zircons[J].Precambrian Research,2004,131(3/4):231-282.
[32]侯可军,李延河,田有荣.LA-MC-ICP-MS锆石微区原位U-Pb定年技术[J].矿床地质,2009,28(4):481-492.
[33]郝爽,李惠民,李国占,等.LA-ICP-MS测定锡石U-Pb同位素年龄时两种普通铅扣除方法的原理及适用性比较[J].地质通报,2016,35(4):622-632.
[34]PUPIN J P.Zircon and granite petrology[J].Contributions to Mineralogy and Petrology,1980,73:207-220.
[35]KOSCHEK G.Origin and significance of the SEM cathodoluminescence from zircon[J].Journal of Microscopy,1993,171:223-232.
[36]WILLGERS B J A,BAKER J A,KROGSTAD E J,et al.Precise and accurate in-situ Pb-Pb dating of apatite,monazite,and sphene by laser ablation multiple-collector ICP-MS[J].Geochimica et Cosmochimica Acta,2002,66(6):1051-1066.
[37]GULSON B L,JONES M T.Cassiterite:potential for direct dating of mineral deposits and a precise age for the Bushveld complex granites[J].Geology,1992,20(4):355-358.
[38]GULSON B L,JONES M T.Cassiterite:potential for direct dating of mineral deposits and a precise age for the Bushveld complex granites:comment and reply[J].Geology,1993,21(3):286-286.
[39]YUAN S D,PENG J T,HAO S,et al.A precise U-Pb age on cassiterite from the Xianghualing tin-polymetallic deposit(Hunan,South China)[J].Mineralium Deposita,2008,43(4):375-382.
[40]PLIMER I R,LU J,KLEEMAN J D.Trace and rare earth elements in cassiterite sources of components for the tin deposits of the Mole granite,Australia[J].Mineralium Deposita,1991,26:267-274.
[41]刘玉平,李正祥,李惠民,等.都龙锡锌矿床锡石和锆石U-Pb年代学:滇东南白垩纪大规模花岗岩成岩-成矿事件[J].岩石学报,2007,23(5):967-976.
[42]WANG Z Q,CHEN B,MA X H.In-situ LA-ICP-MS U-Pb ages and geochemical data of cassiterite from the Furong tin deposit,the Nanling Range:implications for the origin and evolution of the ore-forming fluid[J].Chinese Science Bulletin,2014,59(25):2505-2519.
[43]杜安道,屈文俊,王登红,等.辉钼矿亚晶粒范围内Re和187 Os的失耦现象[J].矿床地质,2007,26(5):572-580.
[44]艾永富,张晓辉.内蒙古大井矿床的脉岩与成矿[C]∥中国地质学会.“八五”地质科技重要成果学术交流会论文集.北京:冶金工业出版社,1996:231-234.
[45]王国政.内蒙古安乐锡铜矿床地质特征及成因[J].矿床地质,1997,16(3):69-80.
[46]王国政.宝盖沟锡矿:黑英岩钠长岩型高温热液矿床[J].地质与勘探,2002,38(2):42-45.
[47]周振华,吕林素,冯佳睿,等.内蒙古黄岗夕卡岩型锡铁矿床辉钼矿Re-Os年龄及其地质意义[J].岩石学报,2010,26(3):667-679.
[48]翟德高,刘家军,杨永强,等.内蒙古黄岗梁铁锡矿床成岩、成矿时代与构造背景[J].岩石矿物学杂志,2012,31(4):513-523.
[49]王明艳,何玲.内蒙古查木罕钨钼多金属矿床辉钼矿Re-Os同位素年龄及其地质意义[J].大地构造与成矿学,2013,37(1):49-56.
[50]廖震,王玉往,王京彬,等.内蒙古大井锡多金属矿床锡石LA-MC-ICP-MS U-Pb测年及其意义[J].矿床地质,2014,(S1):421-422.
[51]王承洋.内蒙古黄岗梁-甘珠尔庙成矿带铅锌多金属成矿系列与找矿方向[D].长春:吉林大学,2015:1-167.
[52]要梅娟,曹烨,刘家军,等.内蒙古黄岗梁铁锡矿床辉钼矿Re-Os年龄及其成因意义[J].矿产勘查,2016,7(3):399-403.
[53]艾霞,冯建忠.内蒙古大井银锡多金属矿床成矿地质特征及成因探讨[J].有色金属矿产与勘查,1992,1(2):82-92.
[54]张德全.敖瑙达巴斑岩型锡多金属矿床地质特征[J].矿床地质,1993,12(1):10-19.
[55]芮宗瑶.华北陆块北缘及邻区有色金属矿床地质[M].北京:地质出版社,1994:1-576.
[56]刘玉强.内蒙古毛登锡铜矿床地质及成因[J].矿床地质,1996,15(2):133-143.
[57]毛骞.内蒙古黄岗矿集区与锡矿化有关的花岗岩成因研究[D].北京:中国科学院地质与地球物理研究所,2001:1-74.
[58]刘伟,潘小菲,谢烈文,等.大兴安岭南段林西地区花岗岩类的源岩:地壳生长的时代和方式[J].岩石学报,2007,23(2):441-460.
[59]江思宏,聂凤军,白大明,等.内蒙古白音诺尔铅锌矿床印支期成矿的年代学证据[J].矿床地质,2011,30(5):787-798.
[60]阮班晓,吕新彪,刘申态,等.内蒙古边家大院铅锌银矿床成因:来自锆石U-Pb年龄和多元同位素的制约[J].矿床地质,2013,32(3):501-514.
[61]姚磊,吕志成,叶天竺,等.大兴安岭南段内蒙古白音查干Sn多金属矿床石英斑岩的锆石U-Pb年龄、地球化学和NdHf同位素特征及地质意义[J].岩石学报,2017,28(2):3183-3199.
[62]周振华.内蒙古黄岗锡铁矿床地质与地球化学[D].北京:中国地质科学院,2011:1-182.
[63]陈毓川.矿床的成矿系列[J].地学前缘,1994,1(3):90-94.
[64]陈毓川,裴荣富,王登红.三论矿床的成矿系列问题[J].地质学报,2006,80(10):1501-1508.
[65]武广,王国瑞,刘军,等.大兴安岭北部主要金属矿床成矿系列和区域矿床成矿谱系[J].矿床地质,2014,33(6):1127-1150.
[66]张家菁,陈郑辉,王登红,等.福建行洛坑大型钨矿的地质特征、成矿时代及其找矿意义[J].大地构造与成矿学,2008,32(1):92-97.
[67]李胜虎,李建康,张德会,等.广西栗木钽铌锡多金属矿床的成矿流体演化及其对成矿过程的制约[J].岩石学报,2015,31(4):954-966.
[68]李光来,华仁民,黄小娥,等.赣中下桐岭钨矿辉钼矿Re-Os年龄及其地质意义[J].矿床地质,2011,30(6):1075-1084.
[69]DAVIS G A,WANG C,ZHENG Y D,et al.The enigmatic Yinshan fold-and-thrust belt of northern China:new views on its intraplate contractional styles[J].Geology,1998,26:43-46.
[70]李锦轶,莫申国,和政军,等.大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约[J].地学前缘,2004,11(3):157-167.
[71]陈衍景,张成,李诺,等.中国东北钼矿床地质[J].吉林大学学报(地球科学版),2012,42(5):1223-1268.
[72]CHEN Y J,ZHANG C,WANG P,et al.The Mo deposits of Northeast China:apowerful indicator of tectonic settings and associated evolutionary trends[J].Ore Geology Reviews,2017,81(2):602-640.
[73]MAO J W,WANG Y T,ZHANG Z H,et al.Geodynamic settings of Mesozoic large-scale mineralization in the North China and adjacent areas:implication from the highly precise and accurate ages of metal deposits[J].Science in China:Series D,2003,33:838-851.
[74]赵越,徐刚,张拴宏,等.燕山运动与东亚构造体制的转变[J].地学前缘,2004,11(3):319-328.
[75]GE W C,WU F Y,ZHOU C Y,et al.Porphyry Cu-Mo deposits in the eastern Xing’an-Mongolian Orogenic Belt:mineralization ages and their geodynamic implications[J].Chinese Science Bulletin,2007,52:3416-3427.
[76]XU W L,PEI F P,WANG F,et al.Spatial-temporal relationships of Mesozoic volcanic rocks in NE China:constraints on tectonic overprinting and transformations between multiple tectonic regimes[J].Journal of Asian Earth Sciences,2013,74:167-193.
[77]ZHAI M G,ZHU R X,LIU J M,et al.Time range of Mesozoic tectonic regime inversion in eastern North China Block[J].Science in China:Series D,2004,47:151-159.
[78]MAO J W,PIRAJNO F,XIANG J F,et al.Mesozoic molybdenum deposits in the East Qinling-Dabie orogenic belt:characteristics and tectonic settings[J].Ore Geology Reviews,2001,43:264-293.
[79]WU G,LI X Z,XU L Q,et al.Age,geochemistry,and SrNd-Hf-Pb isotopes of the Caosiyao porphyry Mo deposit in Inner Mongolia,China[J].Ore Geology Reviews,2017,81:706-727.
[80]KRAVCHINSKY V A,COGNE J P,HARBERT,et al.Evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone,Siberia[J].Geophysical Journal International,2002,148:34-57.
[81]MENG Q R.What drove late Mesozoic extension of the northern China-Mongolia tract?[J].Tectonophysics,2003,369:155-174.
[2]赵一鸣,张德全.大兴安岭及其邻区铜多金属矿床成矿规律与远景评价[M].北京:地震出版社,1997:1-318.
[3]毛景文,周振华,武广,等.内蒙古及邻区矿床成矿规律与成矿系列[J].矿床地质,2013,32(4):716-730.
[4]陈郑辉,王登红,盛继福,等.中国锡矿成矿规律概要[J].地质学报,2015,89(6):1026-1037.
[5]OUYANG H G,MAO J W,ZHOU Z H,et al.Late Mesozoic metallogeny and intracontinental magmatism,southern Great Xing’an Range,northeastern China[J].Gondwana Research,2015,27(3):1153-1172.
[6]王春女,王全明,于晓飞,等.大兴安岭南段锡矿成矿特征及找矿前景[J].地质与勘探,2016,52(2):220-227.
[7]ZHOU Z H,MAO J W,LYCKBERG P,et al.Geochronology and isotopic geochemistry of the A-type granites from the Huanggang Sn-Fe deposit,southern Great Hinggan Range,NE China:implication for their origin and tectonic setting[J].Journal of Asian Earth Sciences,2012,49(3):272-286.
[8]LIU Y F,JIANG S H,BAGAS L.The genesis of metal zonation in the Weilasituo and Bairendaba Ag-Zn-Pb-Cu-(SnW)deposits in the shallow part of a porphyry Sn-W-Rb system,Inner Mongolia,China[J].Ore Geology Reviews,2016,75(2):150-173.
[9]WANG F X,BAGAS L,JIANG S H,et al.Geological,geochemical,and geochronological characteristics of Weilasituo Sn-polymetal deposit,Inner Mongolia,China[J].Ore Geology Reviews,2017,80:1206-1229.
[10]江思宏,聂凤军,刘翼飞,等.内蒙古拜仁达坝及维拉斯托银多金属矿床的硫和铅同位素研究[J].矿床地质,2010,28(1):101-112.
[11]OUYANG H G,MAO J W,SANTOSH M,et al.The early Cretaceous Weilasituo Zn-Cu-Ag vein deposit in the southern Great Xing’an Range,northeast China:fluid inclusions,H,O,S,Pb isotope geochemistry and genetic implications[J].Ore Geology Reviews,2014,56:503-515.
[12]内蒙古维拉斯托矿业有限责任公司,内蒙古地质勘查有限责任公司.内蒙古自治区克什克腾旗维拉斯托矿区锡多金属矿勘探报告[R].呼和浩特:内蒙古自治区地质调查院,2015:1-112.
[13]王瑾,侯青叶,陈岳龙,等.内蒙古维拉斯托铜多金属矿床流体包裹体研究[J].现代地质,2010,24(5):847-855.
[14]申伍军,王学求,聂兰仕.大兴安岭成矿带大型银多金属矿区域地球化学预测指标[J].地学前缘,2012,19(3):49-58.
[15]刘翼飞,聂凤军,江思宏,等.内蒙古拜仁达坝铅-锌-银矿床:元素分带及其成因[J].吉林大学学报(地球科学版),2012,42(4):1055-1068.
[16]刘翼飞,樊志勇,蒋胡灿,等.内蒙古维拉斯托-拜仁达坝斑岩-热液脉状成矿体系研究[J].地质学报,2014,88(12):2373-2385.
[17]欧阳荷根.大兴安岭南段拜仁达坝-维拉斯托银多金属矿床成矿作用及动力学背景[D].北京:中国地质大学(北京),2013:1-192.
[18]梅微,吕新彪,唐然坤,等.大兴安岭南段西坡拜仁达坝-维拉斯托矿床成矿流体特征及其演化[J].地球科学:中国地质大学学报,2015,40(1):145-162.
[19]潘小菲,郭利军,王硕,等.内蒙古维拉斯托铜锌矿床的白云母Ar/Ar年龄探讨[J].岩石矿物学杂志,2009,28(5):473-479.
[20]翟德高,刘家军,李俊明,等.内蒙古维拉斯托斑岩型锡矿床成岩、成矿时代及其地质意义[J].矿床地质,2016,35(5):1011-1022.
[21]郭贵娟.内蒙古维拉斯托锡多金属矿床地质特征及成因探讨[D].北京:中国地质大学(北京),2016:1-70.
[22]祝新友,张志辉,付旭,等.内蒙古赤峰维拉斯托大型锡多金属矿的地质地球化学特征[J].中国地质,2016,43(1):188-208.
[23]王瑾.内蒙古维拉斯托铜多金属矿床矿区花岗岩类年代学与地球化学[D].北京:中国地质大学(北京),2009:1-68.
[24]王新宇,侯青叶,王瑾,等.内蒙古维拉斯托矿床花岗岩类SHRIMP年代学及Hf同位素研究[J].现代地质,2013,27(1):67-78.
[25]薛怀民,郭利军,侯增谦,等.大兴安岭西南坡成矿带晚古生代中期未变质岩浆岩的SHRIMP锆石U-Pb年代学[J].岩石矿物学杂志,2010,29(6):811-823.
[26]刘翼飞.内蒙古克什克腾旗拜仁达坝银多金属矿床成因研究[D].北京:中国地质科学院,2009:1-98.
[27]樊志勇,邱慧远,付旭,等.内蒙古维拉斯托大型斑岩型锡多金属找矿勘查及启示[J].黄金科技技术,2017,25(1):9-17.
[28]YUAN S D,PENG J T,HU R Z,et al.In-situ LA-MC-ICP-MS and ID-TIMS U-Pb geochronology of cassiterite in the giant Furong tin deposit,Hunan Province,South China:new constraints on the timing of tin-polymetallic mineralization[J].Ore Geology Reviews,2011,43(1):235-242.
[29]ANDERSEN T.Correction of common lead in U-Pb analyses that do not report 204Pb[J].Chemical Geology,2002,192(1):59-79.
[30]LUDWIG K R.Isoplot:aplotting and regression program for radiogenic-isotope data[R].USGS Open-File Report,1997,Version 2.92:91-445.
[31]GRIFFIN W L,BELOUSOVA E A,SHEE S R,et al.Archean crustal evolution in the northern Yilgarn Craton:U-Pb and Hf-isotope evidence from detrital zircons[J].Precambrian Research,2004,131(3/4):231-282.
[32]侯可军,李延河,田有荣.LA-MC-ICP-MS锆石微区原位U-Pb定年技术[J].矿床地质,2009,28(4):481-492.
[33]郝爽,李惠民,李国占,等.LA-ICP-MS测定锡石U-Pb同位素年龄时两种普通铅扣除方法的原理及适用性比较[J].地质通报,2016,35(4):622-632.
[34]PUPIN J P.Zircon and granite petrology[J].Contributions to Mineralogy and Petrology,1980,73:207-220.
[35]KOSCHEK G.Origin and significance of the SEM cathodoluminescence from zircon[J].Journal of Microscopy,1993,171:223-232.
[36]WILLGERS B J A,BAKER J A,KROGSTAD E J,et al.Precise and accurate in-situ Pb-Pb dating of apatite,monazite,and sphene by laser ablation multiple-collector ICP-MS[J].Geochimica et Cosmochimica Acta,2002,66(6):1051-1066.
[37]GULSON B L,JONES M T.Cassiterite:potential for direct dating of mineral deposits and a precise age for the Bushveld complex granites[J].Geology,1992,20(4):355-358.
[38]GULSON B L,JONES M T.Cassiterite:potential for direct dating of mineral deposits and a precise age for the Bushveld complex granites:comment and reply[J].Geology,1993,21(3):286-286.
[39]YUAN S D,PENG J T,HAO S,et al.A precise U-Pb age on cassiterite from the Xianghualing tin-polymetallic deposit(Hunan,South China)[J].Mineralium Deposita,2008,43(4):375-382.
[40]PLIMER I R,LU J,KLEEMAN J D.Trace and rare earth elements in cassiterite sources of components for the tin deposits of the Mole granite,Australia[J].Mineralium Deposita,1991,26:267-274.
[41]刘玉平,李正祥,李惠民,等.都龙锡锌矿床锡石和锆石U-Pb年代学:滇东南白垩纪大规模花岗岩成岩-成矿事件[J].岩石学报,2007,23(5):967-976.
[42]WANG Z Q,CHEN B,MA X H.In-situ LA-ICP-MS U-Pb ages and geochemical data of cassiterite from the Furong tin deposit,the Nanling Range:implications for the origin and evolution of the ore-forming fluid[J].Chinese Science Bulletin,2014,59(25):2505-2519.
[43]杜安道,屈文俊,王登红,等.辉钼矿亚晶粒范围内Re和187 Os的失耦现象[J].矿床地质,2007,26(5):572-580.
[44]艾永富,张晓辉.内蒙古大井矿床的脉岩与成矿[C]∥中国地质学会.“八五”地质科技重要成果学术交流会论文集.北京:冶金工业出版社,1996:231-234.
[45]王国政.内蒙古安乐锡铜矿床地质特征及成因[J].矿床地质,1997,16(3):69-80.
[46]王国政.宝盖沟锡矿:黑英岩钠长岩型高温热液矿床[J].地质与勘探,2002,38(2):42-45.
[47]周振华,吕林素,冯佳睿,等.内蒙古黄岗夕卡岩型锡铁矿床辉钼矿Re-Os年龄及其地质意义[J].岩石学报,2010,26(3):667-679.
[48]翟德高,刘家军,杨永强,等.内蒙古黄岗梁铁锡矿床成岩、成矿时代与构造背景[J].岩石矿物学杂志,2012,31(4):513-523.
[49]王明艳,何玲.内蒙古查木罕钨钼多金属矿床辉钼矿Re-Os同位素年龄及其地质意义[J].大地构造与成矿学,2013,37(1):49-56.
[50]廖震,王玉往,王京彬,等.内蒙古大井锡多金属矿床锡石LA-MC-ICP-MS U-Pb测年及其意义[J].矿床地质,2014,(S1):421-422.
[51]王承洋.内蒙古黄岗梁-甘珠尔庙成矿带铅锌多金属成矿系列与找矿方向[D].长春:吉林大学,2015:1-167.
[52]要梅娟,曹烨,刘家军,等.内蒙古黄岗梁铁锡矿床辉钼矿Re-Os年龄及其成因意义[J].矿产勘查,2016,7(3):399-403.
[53]艾霞,冯建忠.内蒙古大井银锡多金属矿床成矿地质特征及成因探讨[J].有色金属矿产与勘查,1992,1(2):82-92.
[54]张德全.敖瑙达巴斑岩型锡多金属矿床地质特征[J].矿床地质,1993,12(1):10-19.
[55]芮宗瑶.华北陆块北缘及邻区有色金属矿床地质[M].北京:地质出版社,1994:1-576.
[56]刘玉强.内蒙古毛登锡铜矿床地质及成因[J].矿床地质,1996,15(2):133-143.
[57]毛骞.内蒙古黄岗矿集区与锡矿化有关的花岗岩成因研究[D].北京:中国科学院地质与地球物理研究所,2001:1-74.
[58]刘伟,潘小菲,谢烈文,等.大兴安岭南段林西地区花岗岩类的源岩:地壳生长的时代和方式[J].岩石学报,2007,23(2):441-460.
[59]江思宏,聂凤军,白大明,等.内蒙古白音诺尔铅锌矿床印支期成矿的年代学证据[J].矿床地质,2011,30(5):787-798.
[60]阮班晓,吕新彪,刘申态,等.内蒙古边家大院铅锌银矿床成因:来自锆石U-Pb年龄和多元同位素的制约[J].矿床地质,2013,32(3):501-514.
[61]姚磊,吕志成,叶天竺,等.大兴安岭南段内蒙古白音查干Sn多金属矿床石英斑岩的锆石U-Pb年龄、地球化学和NdHf同位素特征及地质意义[J].岩石学报,2017,28(2):3183-3199.
[62]周振华.内蒙古黄岗锡铁矿床地质与地球化学[D].北京:中国地质科学院,2011:1-182.
[63]陈毓川.矿床的成矿系列[J].地学前缘,1994,1(3):90-94.
[64]陈毓川,裴荣富,王登红.三论矿床的成矿系列问题[J].地质学报,2006,80(10):1501-1508.
[65]武广,王国瑞,刘军,等.大兴安岭北部主要金属矿床成矿系列和区域矿床成矿谱系[J].矿床地质,2014,33(6):1127-1150.
[66]张家菁,陈郑辉,王登红,等.福建行洛坑大型钨矿的地质特征、成矿时代及其找矿意义[J].大地构造与成矿学,2008,32(1):92-97.
[67]李胜虎,李建康,张德会,等.广西栗木钽铌锡多金属矿床的成矿流体演化及其对成矿过程的制约[J].岩石学报,2015,31(4):954-966.
[68]李光来,华仁民,黄小娥,等.赣中下桐岭钨矿辉钼矿Re-Os年龄及其地质意义[J].矿床地质,2011,30(6):1075-1084.
[69]DAVIS G A,WANG C,ZHENG Y D,et al.The enigmatic Yinshan fold-and-thrust belt of northern China:new views on its intraplate contractional styles[J].Geology,1998,26:43-46.
[70]李锦轶,莫申国,和政军,等.大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演化重建的制约[J].地学前缘,2004,11(3):157-167.
[71]陈衍景,张成,李诺,等.中国东北钼矿床地质[J].吉林大学学报(地球科学版),2012,42(5):1223-1268.
[72]CHEN Y J,ZHANG C,WANG P,et al.The Mo deposits of Northeast China:apowerful indicator of tectonic settings and associated evolutionary trends[J].Ore Geology Reviews,2017,81(2):602-640.
[73]MAO J W,WANG Y T,ZHANG Z H,et al.Geodynamic settings of Mesozoic large-scale mineralization in the North China and adjacent areas:implication from the highly precise and accurate ages of metal deposits[J].Science in China:Series D,2003,33:838-851.
[74]赵越,徐刚,张拴宏,等.燕山运动与东亚构造体制的转变[J].地学前缘,2004,11(3):319-328.
[75]GE W C,WU F Y,ZHOU C Y,et al.Porphyry Cu-Mo deposits in the eastern Xing’an-Mongolian Orogenic Belt:mineralization ages and their geodynamic implications[J].Chinese Science Bulletin,2007,52:3416-3427.
[76]XU W L,PEI F P,WANG F,et al.Spatial-temporal relationships of Mesozoic volcanic rocks in NE China:constraints on tectonic overprinting and transformations between multiple tectonic regimes[J].Journal of Asian Earth Sciences,2013,74:167-193.
[77]ZHAI M G,ZHU R X,LIU J M,et al.Time range of Mesozoic tectonic regime inversion in eastern North China Block[J].Science in China:Series D,2004,47:151-159.
[78]MAO J W,PIRAJNO F,XIANG J F,et al.Mesozoic molybdenum deposits in the East Qinling-Dabie orogenic belt:characteristics and tectonic settings[J].Ore Geology Reviews,2001,43:264-293.
[79]WU G,LI X Z,XU L Q,et al.Age,geochemistry,and SrNd-Hf-Pb isotopes of the Caosiyao porphyry Mo deposit in Inner Mongolia,China[J].Ore Geology Reviews,2017,81:706-727.
[80]KRAVCHINSKY V A,COGNE J P,HARBERT,et al.Evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone,Siberia[J].Geophysical Journal International,2002,148:34-57.
[81]MENG Q R.What drove late Mesozoic extension of the northern China-Mongolia tract?[J].Tectonophysics,2003,369:155-174.