论兴蒙造山带叠生成矿作用——以锡林浩特和额尔古纳地块为例
|
摘要
兴蒙造山带前寒武纪变质岩中间地块分布广泛,其中锡林浩特和额尔古纳地块以出露范围广泛、岩性组合复杂、后期改造明显和找矿潜力巨大而为人们所关注。找矿勘查结果表明,锡林浩特和额尔古纳地块及邻区铜、铁、铅-锌和银矿床(点)星罗棋布,并且以含有大量锡、钨和钼为特征。这些矿床独特的成矿元素组合(如铜-锡、铁-锡、铜-锡-铅-锌-银、铜-银-锡和铁-钨-钼)及其与前寒武纪变质岩块体和显生宙花岗岩密切时空分布关系均表明,它们很可能是深源岩浆再造和古陆块体活化相互联动(叠生)作用的产物。所谓的叠生作用主要指地壳浅部构造形迹活化和地壳深部物质再造,前者为成岩(矿)物质的就位提供了空间条件,后者为岩(矿)体的形成的奠定了物质基础。钕和铪同位素数据表明,前寒武纪变质岩块体和显生宙含锡、钨和钼花岗岩分别具有完全不同的εNd(t)值和εHf(t)值,成岩(矿)物质分别属于壳源和幔源,其中后者对前者的叠加改造是导致铜-锡、铁-锡和铜-银-锡等多元素矿床形成的关键因素。叠生成矿作用概念的提出不仅很好地解释了兴蒙造山带含锡、钨和钼多金属矿床的成因,而且为寻找隐伏金属矿床指明了方向。
Precambrian metamorphic intermediate massifs are widely distributed in the Da Hinggan-Mongolia Paleozoic orogenic belt,among which the Xilinhot and Ergun massifs are the largest ones,and show a complex rejuvenation history. Mineral exploration and regional metallogenic studies show that Sn-,W- and Mo-polymetallic deposits are well developed both in the Xilinhot and Ergun massifs,and can be classified into five types in term of their host rocks and metallogenic features. They are( 1) porphyry type Sn,W( Mo) and Cu( Mo) deposits;( 2) skarn type Sn-Fe and Sn-Ag-Cu deposits;( 3) shallow-emplaced granitoid intrusive dykes( swarms)-related vein type Sn,Wand Mo-W deposits;( 4) deep-seated emplaced granitoid intrusive stocks( batholiths)-related vein type Sn,W and Mo deposits;( 5) felsic volcanic type Sn deposits. Among all the five type deposits,the first two bear the most important economic significance. It has been noted that Sn-,W- and Mo-polymetallic mineralization occurs within the Precambrian metamorphic massifs,but they have an intimate spatial and temporal relationship with Mesozoic granitoid intrusions. In general,Sn,W and Mo are considered as the continent-affiliation elements,while Cu,Ni,Au and PGE are derived from the mantle-relate magmatic and its related or hydrothermal sources. Preliminary studies show that the rejuvenation of pre-existing crust and lithosphere or /and mantle may be the important factor for the regional metallogenesis of Sn-,W-and Mo-polymetallic deposits occurring within the Xilinhot and Ergun intermediate massifs. The rejuvenation occurs largely via two related processes: reactivation and re-working. The reactivation is normally considered to involve the rejuvenation of discrete structures,whilst reworking involves the repeated focusing of metamorphism,deformation and magmatism into the same crustal- or lithospheric-scale volume. Melting of existing continental lithosphere( mantle) is a dramatic thermal expression of reworking. However,the emplacement of the granitoid magma commonly exploits pre-existing structures and may promote transient fault weakening during emplacement. Thus the vastly different processes of magma generation( reworking) and emplacement( reactivation) are both essentially expressions of the thermal rejuvenation of existing continental lithosphere. Our Nd-Sr-Pb isotopic studies show that the ore-forming materials,dynamic force and fluids may be provided by the Mesozoic granitoid magma. Moreover,the accumulation conditions of the ore-forming materials were given by the reactivation of previous-exist faults and fracture zones. The Mesozoic lithosphere stretching and asthenosphere upwelling may result in the reworking of continental crust( Precambrian metamorphic intermediate massifs) and primitive crust( previously formed mafic igneous rocks with positive εNd( t) and εHf( t) values),and then produced Sn-,W-,and Mo-rich granitoid magma. When the magma moved along reactivated structures developed within the Precambrian metamorphic intermediate massifs,ore-bearing fluids derived from condensation fraction of the granitoid magma filled the structures and replaced country rock,thus forming the Sn-,W-,and Mo-polymetallic deposits. Therefore,it is believed that the all the deposits are the products of the Mesozoic intraplate granitoid magmatic occurring in the Xilinhot and Ergun intermediate massifs. Moreover,the intensive superimposition of the Mesozoic tectono-magmatic events and the Precambrian metamorphic massifs may greatly upgrade the enrichment of the Sn-,W- and Mo-polymetallic elements. The rejuvenated metallogenic model and mineral exploration criteria of the Sn,W and Mo-polymetallic deposits can also be used as useful tool during the comprehensive evaluation of concealed deposits in the Da Hinggan-Mongolia Paleozoic orogenic belt.
Precambrian metamorphic intermediate massifs are widely distributed in the Da Hinggan-Mongolia Paleozoic orogenic belt,among which the Xilinhot and Ergun massifs are the largest ones,and show a complex rejuvenation history. Mineral exploration and regional metallogenic studies show that Sn-,W- and Mo-polymetallic deposits are well developed both in the Xilinhot and Ergun massifs,and can be classified into five types in term of their host rocks and metallogenic features. They are( 1) porphyry type Sn,W( Mo) and Cu( Mo) deposits;( 2) skarn type Sn-Fe and Sn-Ag-Cu deposits;( 3) shallow-emplaced granitoid intrusive dykes( swarms)-related vein type Sn,Wand Mo-W deposits;( 4) deep-seated emplaced granitoid intrusive stocks( batholiths)-related vein type Sn,W and Mo deposits;( 5) felsic volcanic type Sn deposits. Among all the five type deposits,the first two bear the most important economic significance. It has been noted that Sn-,W- and Mo-polymetallic mineralization occurs within the Precambrian metamorphic massifs,but they have an intimate spatial and temporal relationship with Mesozoic granitoid intrusions. In general,Sn,W and Mo are considered as the continent-affiliation elements,while Cu,Ni,Au and PGE are derived from the mantle-relate magmatic and its related or hydrothermal sources. Preliminary studies show that the rejuvenation of pre-existing crust and lithosphere or /and mantle may be the important factor for the regional metallogenesis of Sn-,W-and Mo-polymetallic deposits occurring within the Xilinhot and Ergun intermediate massifs. The rejuvenation occurs largely via two related processes: reactivation and re-working. The reactivation is normally considered to involve the rejuvenation of discrete structures,whilst reworking involves the repeated focusing of metamorphism,deformation and magmatism into the same crustal- or lithospheric-scale volume. Melting of existing continental lithosphere( mantle) is a dramatic thermal expression of reworking. However,the emplacement of the granitoid magma commonly exploits pre-existing structures and may promote transient fault weakening during emplacement. Thus the vastly different processes of magma generation( reworking) and emplacement( reactivation) are both essentially expressions of the thermal rejuvenation of existing continental lithosphere. Our Nd-Sr-Pb isotopic studies show that the ore-forming materials,dynamic force and fluids may be provided by the Mesozoic granitoid magma. Moreover,the accumulation conditions of the ore-forming materials were given by the reactivation of previous-exist faults and fracture zones. The Mesozoic lithosphere stretching and asthenosphere upwelling may result in the reworking of continental crust( Precambrian metamorphic intermediate massifs) and primitive crust( previously formed mafic igneous rocks with positive εNd( t) and εHf( t) values),and then produced Sn-,W-,and Mo-rich granitoid magma. When the magma moved along reactivated structures developed within the Precambrian metamorphic intermediate massifs,ore-bearing fluids derived from condensation fraction of the granitoid magma filled the structures and replaced country rock,thus forming the Sn-,W-,and Mo-polymetallic deposits. Therefore,it is believed that the all the deposits are the products of the Mesozoic intraplate granitoid magmatic occurring in the Xilinhot and Ergun intermediate massifs. Moreover,the intensive superimposition of the Mesozoic tectono-magmatic events and the Precambrian metamorphic massifs may greatly upgrade the enrichment of the Sn-,W- and Mo-polymetallic elements. The rejuvenated metallogenic model and mineral exploration criteria of the Sn,W and Mo-polymetallic deposits can also be used as useful tool during the comprehensive evaluation of concealed deposits in the Da Hinggan-Mongolia Paleozoic orogenic belt.
引文
Belousov BB.1955.Basic problems of the tectonics.Acta GeologicaSinica,35(3):177-189(in Chinese with English abstract)
Blatt H and Jones RL.1975.Proportions of exposed igneous,metamorphic,and sedimentary rocks.Geological Society of AmericaBulletin,86(8):1085-1088
Chen GD.1956.Examples of“activating region”in the Chinese platformwith special reference to the“Cathaysia”problem.Acta GeologicaSinica,36(3):239-271(in Chinese with English abstract)
Chen GD.1959.The third basic tectonic unit of the crust:Diwa district.Chinese Science Bulletin,(3):94-95(in Chinese)
Chen GD,Chen JC,Wei BL,Xue JM,Liu YX,Wen SJ,Wei ZL andHu HY.1975.A brief review on the geotectonics of China.ScientiaGeologica Sinica,(3):205-219(in Chinese with Englishabstract)
Chen YJ,Zhang C,Li N,Yang YF and Deng K.2012.Geology of theMo deposits in Northeast China.Journal of Jilin University(EarthScience Edition),42(5):1223-1268(in Chinese with Englishabstract)
Chen ZG,Zhang LC,Lu BZ,Li ZL,Wu HY,Xiang P and Huang SW.2010.Geochronology and geochemistry of the Taipingchuan coppermolybdenum deposit in Inner Mongolia,and its geologicalsignificances.Acta Petrologica Sinica,26(5):1437-1449(inChinese with English abstract)
Chen ZG,Zhang LC,Wan B,Wu HY and Cleven N.2011.Geochronology and geochemistry of the Wunugetushan porphyry CuMo deposit in NE China,and their geological significance.OreGeology Reviews,43(1):92-105
Du BF,Wei JH,Wang Q,Li YJ,Liu GC,Yu HT and Liu YL.2010.Discussion on metallogenic setting and time difference betweenmagmatism and mineralization of molybdenum deposits in EastChina.Mineral Deposits,29(6):935-955(in Chinese withEnglish abstract)
Groves DI and Bierlein FP.2007.Geodynamic settings of mineral depositsystems.Journal of the Geological Society,164(1):19-30
Hao X and Xu B.1997.Sm-Nd,Rb-Sr isotopic geochronology of theXilin Gol complex,Inner Mongolia,China.Geological Review,43(1):101-105(in Chinese with English abstract)
Holdsworth RE,Handa M,Miller JA and Buick IS.2001.Continentalreactivation and reworking:An introduction.Geological Society,London,Special Publications,184(1):1-12
Hong DW,Wang SG,Xie XL and Zhang JS.2000.Genesis of positiveεNd(t)granitoids in the Da Hinggan Mts.-Mongolia orogenic beltand growth continental crust.Earth Science Frontiers,7(2):441-456(in Chinese with English abstract)
Hong DW,Wang SG,Xie XL,Zhang JS and Wang T.2003.Metallogenic province derived from mantle sources:A case study ofcentral Asian orogenic belt.Mineral Deposits,22(1):41-55(inChinese with English abstract)
Hou ZQ,Zheng YC,Yang ZM and Yang ZS.2012.Metallogenesis ofcontinental collision setting:Part I.Gangdese Cenozoic porphyry CuMo systems in Tibet.Mineral Deposits,31(4):647-670(inChinese with English abstract)
Hurley PM and Rand JR.1969.Pre-drift continental nuclei.Science,164(3885):1229-1242
Bureau of Geology and Mineral Resources of Inner Mongolia AutonomousRegion(BGMRI).1991.Regional Geology of Inner MongoliaAutonomous Region.Beijing:Geol.Pub.House,1-725(inChinese with English abstract)
Jacobsen SB.1988.Isotopic constraints on crustal growth and recycling.Earth and Planetary Science Letters,90(3):315-329
Jia PP,Wei JH,Gong QW and Zhao WL.2011.Analysis of geologicalbackground and ore-searching prospect for the copper-molybdenumdeposits in the Da Hingan Ling area.Geology and Exploration,47(2):151-162(in Chinese with English abstract)
Jiang SH,Nie FJ,Bai DM,Liu YF and Liu Y.2011.Geochronologyevidence for Indosinian mineralization in Baiyinnuoer Pb-Zn depositof Inner Mongolia.Mineral Deposits,30(5):787-798(inChinese with English abstract)
Li JY,Zhang J,Yang TN,Li YP,Sun GH,Zhu ZX and Wang LJ.2009.Crustal tectonic division and evolution of the southern part ofthe North Asian orogenic region and its adjacent areas.Journal ofJilin University(Earth Science Edition),39(4):584-605(inChinese with English abstract)
Li SL and Ouyang ZY.1998.Tectonic framework and evolution of Xing’anling-Mongolian Orogenic Belt(XMOB)and its adjacent region.Marine Geology and Quaternary Geology,18(3):45-54(inChinese with English abstract)
Liu YF,Nie FJ,Jiang SH et al.2010.The geochronology andgeochemical features of ore-hosting granite in the Aryn Nuurmolybdenum deposit,Mongolia.Acta Geoscientica Sinica,31(3):343-349(in Chinese with English abstract)
Ma XH,Chen B,Lai Y and Lu YH.2009.Petrogenesis andmineralization chronology study on the Aolunhua porphyry Modeposit,Inner Mongolia,and its geological implications.ActaPetrologica Sinica,25(11):2939-2950(in Chinese with Englishabstract)
Meng QR.2003.What drove Late Mesozoic extension of the northernChina-Mongolia tract?Tectonophysics,369(3-4):155-174
Nie FJ,Jiang SH,Zhang Y,Liu Y and Hu P.2004.Geological featuresand origin of porphyry copper deposits in China-Mongolia borderregion and its neighboring areas.Mineral Deposits,23(2):176-189(in Chinese with English abstract)
Nie FJ,Jiang SH,Zhang Y,Bai DM,Hu P,Zhao YY,Zhang WY andLiu Y.2007a.Metallogenic Studies and Prospecting Orientation inCentral and Eastern Segments along China-Mongolia.Beijing:Geol.Pub.House,1-574(in Chinese with English abstract)
Nie FJ,Zhang WY,Du AD,Jiang SH and Liu Y.2007b.Re-Os isotopicage dating of molybdenite separates from the Chaobuleng skarn ironpolymetallic deposit,Dong Ujimqin banner,Inner Mongolia.ActaGeoscientica Sinica,28(4):315-323(in Chinese with Englishabstract)
Nie FJ,Jiang SH,Bai DM,Hou WR and Liu YF.2010a.Types andtemporal-spatial distribution of metallic deposits in southern Mongoliaand its neighboring areas.Acta Geoscientica Sinica,31(3):267-288(in Chinese with English abstract)
Nie FJ,Hu P,Jiang SH and Liu YF.2010b.Geological features,geochronology and origin of the tungsten and tungsten(molybdenum)deposits in the Shamai-Yuguzer mineralizationconcentrated camp along the Sino-Mongolian border.ActaGeoscientica Sinica,31(3):383-394(in Chinese with Englishabstract)
Nie FJ and Jiang SH.2011.Geological setting and origin of Mo-W-Cudeposits in the Honggor-Shamai district,Inner Mongolia,NorthChina.Resource Geology,61(4):344-355
Nie FJ,Sun ZJ,Li C,Liu YF,LüKP,Zhang K and Liu Y.2011a.ReOs isotopic dating of molybdenite separates from Chalukou porphyryMo polymetallic deposit in Heilongjiang Province.Mineral Deposits,30(5):828-836(in Chinese with English abstract)
Nie FJ,Zhang K,Liu YF,Jiang SH,Liu Y and Liu Y.2011b.Indosinian magamtic activity and molybdenum,gold mineralizationalong the northern margin of North China craton and adjacent area.Journal of Jilin University(Earth Science Edition),41(6):1651-1666(in Chinese with English abstract)
Nie FJ,Sun ZJ,Liu YF,LüKP,Zhao YA and Cao Y.2013.Mesozoicmultiple magmatic activities and molybdenum mineralization in theChalukou ore district,Da Hinggan mountains.Geology in China,40(1):273-286(in Chinese with English abstract)
Nie XL and Hou WR.2010.The discovery of the Diyanqinamu large-sizeMo-Ag deposit,Inner Mongolia,and its geological significance.ActaGeoscientica Sinica,31(3):469-472(in Chinese with Englishabstract)
Pei RF.1995.Mineral Deposit Models of China.Beijing:GeologicalPublishing House,331-336(in Chinese)
Pirajno F,Ernst RE,Borisenko AS et al.2009.Intraplate magmatism incentral Asia and China and associated metallogeny.Ore GeologyReviews,35(2):114-136
Ren JS,Wang ZX,Chen BW,Jiang CF,Nie BG,Li JY,Xie GL,HeZJ and Liu ZG.1999.The Tectonics of China from A Global View:A Guide to Tectonic Map of China and Adjacent Region.Beijing:Geological Publishing House,1-32
Richards JP.2009.Post subduction porphyry Cu-Au and epithermal Audeposits:Products of remelting of subduction-modified lithosphere.Geology,37(3):247-250
Robert F,Brommecker R,Bourne BT,Dobak PJ,McEwan CJ,RoweRR and Zhou X.2007.Models and exploration methods for majorgold deposit types.In:Milkereit B(ed.).Proceedings ofExploration 07:Fifth Decennial International Conference on MineralExploration,691-711
Shen GY.2008.Geological characteristics and prospecting direction ofHaolihao copper-molybdenum deposit in Arhorqin,Inner Mongolia.Geology and Resources,17(4):273-277(in Chinese with Englishabstract)
Sun JG,Zhang Y,Xing SW,Zhao KQ,Zhang ZJ,Bai LA,Ma YB andLiu YS.2012.Genetic types,ore-forming age and geodynamicsetting of endogenic molybdenum deposits in the eastern edge ofXing-Meng orogenic belt.Acta Petrologica Sinica,28(4):1317-1332(in Chinese with English abstract)
Sun LX,Ren BF,Zhao FQ,Gu YC,Li YF and Liu H.2013a.ZirconU-Pb dating and Hf isotopic compositions of the mesoporterozoicgranitic gneiss in Xilinhot block,Inner Mongolia.GeologicalBulletin of China,32(2-3):327-340(in Chinese with Englishabstract)
Sun LX,Ren BF,Zhao FQ,Ji SP and Geng JZ.2013b.LatePaleoproterozoic magmatic records in the Eerguna massif:Evidencesfrom the zircon U-Pb dating of granitic gneisses.Geological Bulletinof China,32(2-3):341-352(in Chinese with English abstract)
Taylor RG.1979.Geology of Tin Deposits-Developments in EconomicGeology.Oxford,Amsterdam and New York:Elsevier Science Ltd,1-544
Vervoort JD and Blichert-Toft J.1999.Evolution of the depleted mantle:Hf isotope evidence from juvenile rocks through time.Geochimica etCosmochimica Acta,63(3-4):533-556
Wang F,Zhou XH,Zhang LC et al.2006.Late mesozoic volcanism inthe Great Xing’an Range(NE China):Timing and implications forthe dynamic setting of NE Asia.Earth and Planetary Science Letters,251(1-2):179-198
Wang JB,Wang YW,Wang LJ and Uemoto T.2001.Tin-polymetallicmineralization in the southern part of the Da Hinggan Mountains,China.Resource Geology,51(4):283-291
Wang MY and He L.2013.Re-Os dating of molybdenites from ChamuhanW-Mo deposit,Inner Mongolia and its geological implications.Geotectonica et Metallogenia,37(1):49-56(in Chinese withEnglish abstract)
Wang YW,Wang JB,Uemoto T and Wang LJ.2001.Geology andmineralization at the Dajing tin-polymetallic ore deposit,InnerMongolia,China.Resource Geology,51(4):307-320
Wu G,Chen YC,Chen YJ and Zeng QT.2012.Zircon U-Pb ages of themetamorphic supracrustal rocks of the Xinghuadukou Group andgranitic complexes in the Argun massif of the northern Great HingganRange,NE China,and their tectonic implications.Journal of AsianEarth Sciences,49:214-233
Xiang AP,She HQ,Guan JD,Kang YJ,Han ZG,Li JW,Yang YC andGuo ZJ.2014.Study on the metallogenic and diagenetic age ofHonghuaerji tungsten polymetallic deposit in Inner Mongolia.MineralDeposits,33(2):428-439(in Chinese with English abstract)
Xu B,Chen B and Shao JA.1996.Sm-Nd and Rb-Sr geochronologicalstudies on Xilinguole complex.Chinese Science Bulletin,41(2):153-155(in Chinese)
Xu ZG.1997.Tectonic evolution and its controlling factors on the oreforming processes of the in the Da Hinggan mountains and itsadjacent regions.In:Zhao YM and Zhang DQ(eds.).Metallogenyand Prospective Evaluation of Copper-polymetallic Deposits in the DaHinggan Mountains and Its Adjacent Regions.Beijing:SeismologicalPress,1-21(in Chinese)
Xue J,Nie FJ,Dai TG,Peng ES and Liu YF.2010.Re-Os isotopicdating of molybdenite from the Aryn nuur Mo deposit in Mongolia andits geological implications.Acta Geoscientica Sinica,31(3):350-356(in Chinese with English abstract)
Yan C,Sun Y,Lai Y and Ma XH.2011.LA-ICP-MS zircon U-Pb andmolybdenite Re-Os isotope ages and metallogenic geodynamic settingof Banlashan Mo deposit,Inner Mongolia.Mineral Deposits,30(4):616-634(in Chinese with English abstract)
Yang YC.2010.Metallogenic studies and prospecting orientation onDeerbugan metallogenic zone and adjacent area.Post-DoctorResearch Report.Beijing:Chinese Academy of Geological Sciences,1-148(in Chinese with English summary)
Zhang K,Nie FJ,Hou WR,Li C and Liu Y.2012.Re-Os isotopic agedating of molybdenite separates from Hashitu Mo deposit in LinxiCounty of Inner Mongolia and its geological significance.MineralDeposits,31(1):129-138(in Chinese with English abstract)
Zhang LC,Wu HY,Xiang P,Zhang XJ,Chen ZG and Wan B.2010.Ore-forming processes and mineralization of complex tectonic systemduring the Mesozoic:A case from Xilamulun Cu-Mo metallogenicbelt.Acta Petrologica Sinica,26(5):1351-1362(in Chinesewith English abstract)
Zhao YM,Wang DW,Zhang DQ,Fu XZ,Bao XP,Li HN and Ai YF.1994.Ore-controlling Factors and Ore-prospecting Models forCopperpolymetallic Ore Deposits in Southeastern Inner Mongolia.Beijing:Seismological Publishing House,1-234(in Chinese)
Zhao YM and Zhang DQ.1997.Metallogeny and Prospective Evaluationof Copper-polymetallic Deposits in the Da Hinggan Mountains and ItsAdjacent Regions.Beijing:Seismological Press,1-318(inChinese)
Zhou XH,Ying JF,Zhang LC and Zhang YT.2009.The petrogenesis oflate Mesozoic volcanic rock and the contributions from ancient microcontinents:Constraints from the zircon U-Pb dating and Sr-Nd-Pb-Hfisotopic systematics.Earth Science,34(1):1-10(in Chinesewith English abstract)
Zhou ZH.2011.Geology and geochemistry of Huanggang Sn-Fe deposit,Inner Mongolia.Ph.D.Dissertation.Beijing:Chinese Academy ofGeological Sciences,1-182(in Chinese with English summary)
Zhu YF,Sun SH,Mao Q and Zhao G.2004.Geochemistry of theXilingele complex,Inner Mongolia:A historic record from rodiniaaccretion to continental collision after closure of the Paleo-AsianOcean.Geological Journal of China Universities,10(3):343-355(in Chinese with English abstract)
别洛乌索夫.1955.大地构造的基本问题.地质学报,35(3):177-189
陈国达.1956.中国地台“活化区”的实例,并着重讨论“华夏古陆”问题.地质学报,36(3):239-271
陈国达.1959.地壳的第三基本构造单元———地洼区.科学通报,(3):94-95
陈国达,陈家超,魏柏林,薛佳谋,刘以宣,文善继,魏洲龄,胡火炎.1975.中国大地构造简述.地质科学,(3):205-219
陈衍景,张成,李诺,杨永飞,邓轲.2012.中国东北钼矿床地质.吉林大学学报(地球科学版),42(5):1223-1268
陈志广,张连昌,卢百志,李占龙,吴华英,相鹏,黄世武.2010.内蒙古太平川铜钼矿成矿斑岩时代、地球化学及地质意义.岩石学报,26(5):1437-1449
杜保峰,魏俊浩,王启,李艳军,刘国春,于海涛,刘永利.2010.中国东部钼矿成矿背景与成岩-成矿时差讨论.矿床地质,29(6):935-955
郝旭,徐备.1997.内蒙古锡林浩特锡林郭勒杂岩的原岩年代和变质年代.地质评论,43(1):101-105
洪大卫,王式光,谢锡林,张季生.2000.兴蒙造山带正εNd(t)值花岗岩的成因和大陆地壳生长.地学前缘,7(2):441-456
洪大卫,王式光,谢锡林,张季生,王涛.2003.试析地幔来源物质成矿域———以中亚造山带为例.矿床地质,22(1):41-55
侯增谦,郑远川,杨志明,杨竹森.2012.大陆碰撞成矿作用:I.冈底斯新生代斑岩成矿系统.矿床地质,31(4):647-670
贾盼盼,魏俊浩,巩庆伟,赵万莉.2011.大兴安岭地区铜钼矿床成矿区带背景及找矿前景分析.地质与勘探,47(2):151-162
江思宏,聂凤军,白大明,刘翼飞,刘妍.2011.内蒙古白音诺尔铅锌矿床印支期成矿的年代学证据.矿床地质,30(5):787-798
李锦轶,张进,杨天南,李亚萍,孙桂华,朱志新,王励嘉.2009.北亚造山区南部及其毗邻地区地壳构造分区与构造演化.吉林大学学报(地球科学版),39(4):584-605
李双林,欧阳自远.1998.兴蒙造山带及邻区的构造格局与构造演化.海洋地质与第四纪地质,18(3):45-54
刘翼飞,聂凤军,江思宏,薛静,侯万荣,云飞.2010.蒙古国阿林诺尔钼矿床赋矿花岗岩年代学及地球化学特征.地球学报,31(3):343-349
马星华,陈斌,赖勇,鲁颖淮.2009.内蒙古敖仑花斑岩钼矿床成岩成矿年代学及地质意义.岩石学报,25(11):2939-2950
内蒙古自治区地质矿产局.1991.内蒙古自治区区域地质志.北京:地质出版社,1-725
聂凤军,江思宏,张义,刘妍,胡朋.2004.中蒙边境及邻区斑岩型铜矿床地质特征及成因.矿床地质,23(2):176-189
聂凤军,江思宏,张义,白大明,胡朋,赵元艺,张万益,刘妍.2007a.中蒙边境中东段金属矿床成矿规律和找矿方向.北京:地质出版社,1-574
聂凤军,张万益,杜安道,江思宏,刘妍.2007b.内蒙古朝不楞矽卡岩型铁多金属矿床辉钼矿铼-锇同位素年龄及地质意义.地球学报,28(4):315-323
聂凤军,江思宏,白大明,侯万荣,刘翼飞.2010a.蒙古国南部及邻区金属矿床类型及其时空分布特征.地球学报,31(3):267-288
聂凤军,胡朋,江思宏,刘翼飞.2010b.中蒙边境沙麦-玉古兹尔地区钨和钨(钼)矿床地质特征,形成时代和成因机理.地球学报,31(3):383-394
聂凤军,孙振江,李超,刘翼飞,吕克鹏,张可,刘勇.2011a.黑龙江岔路口钼多金属矿床辉钼矿铼-锇同位素年龄及地质意义.矿床地质,30(5):828-836
聂凤军,张可,刘翼飞,江思宏,刘勇,刘妍.2011b.华北克拉通北缘及邻区印支期岩浆活动与钼和金成矿作用.吉林大学学报(地球科学版),41(6):1651-1666
聂凤军,孙振江,刘翼飞,吕克鹏,赵宇安,曹毅.2013.大兴安岭岔路口矿区中生代多期岩浆活动与钼成矿作用.中国地质,40(1):273-286
聂秀兰,侯万荣.2010.内蒙古迪彦钦阿木大型钼-银矿床的发现及地质意义.地球学报,31(3):469-472
裴荣富.1995.中国矿床模式.北京:地质出版社,331-336
沈光银.2008.内蒙古阿鲁科尔沁旗好力宝铜钼矿床地质特征及找矿方向.地质与资源,17(4):273-277
孙景贵,张勇,邢树文,赵克强,张增杰,白令安,马玉波,刘勇胜.2012.兴蒙造山带东缘内生钼矿床的成因类型、成矿年代及成矿动力学背景.岩石学报,28(4):1317-1332
孙立新,任邦方,赵凤清,谷永昌,李艳峰,刘卉.2013a.内蒙古锡林浩特地块中元古代花岗片麻岩的锆石U-Pb年龄和Hf同位素特征.地质通报,32(2-3):327-340
孙立新,任邦方,赵凤清,冀世平,耿建珍.2013b.内蒙古额尔古纳地块古元古代末期的岩浆记录-来自花岗片麻岩的锆石U-Pb年龄证据.地质通报,32(2-3):341-352
王明艳,何玲.2013.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.大地构造与成矿学,37(1):49-56
向安平,佘宏全,关继东,康永建,韩增光,李进文,杨郧城,郭志军.2014.内蒙古红花尔基钨多金属矿成岩成矿年代学研究.矿床地质,33(2):428-439
徐备,陈斌,邵济安.1996.内蒙古锡林郭勒杂岩Sm-Nd,Rb-Sr同位素年代研究.科学通报,41(2):153-155
徐志刚.1997.大兴安岭及其邻区构造演化及控矿作用.见:赵一鸣,张德全主编.大兴安岭及其邻区铜多金属矿床成矿规律与远景评价.北京:地震出版社,1-21
薛静,聂凤军,戴塔根,彭恩生,刘翼飞.2010.蒙古国阿林诺尔钼矿床辉钼矿Re-Os同位素年龄及地质意义.地球学报,31(3):350-356
闫聪,孙艺,赖勇,马星华.2011.内蒙古半拉山钼矿LA-ICP-MS锆石U-Pb与辉钼矿Re-Os年龄及其成矿动力学背景.矿床地质,30(4):616-634
杨郧城.2010.得尔布干成矿带及邻区成矿规律与找矿方向研究.博士后研究工作报告.北京:中国地质科学院,1-148
张可,聂凤军,侯万荣,李超,刘勇,2012.内蒙古林西县哈什吐钼矿床辉钼矿铼-锇年龄及其地质意义.矿床地质,31(1):129-138
张连昌,吴华英,相鹏,张晓静,陈志广,万博.2010.中生代复杂构造体系的成矿过程与成矿作用:以华北大陆北缘西拉木伦钼铜多金属成矿带为例.岩石学报,26(5):1351-1362
赵一鸣,王大畏,张德全,傅先政,鲍修坡,李鹤年,艾永富.1994.内蒙古东南部铜多金属成矿地质条件及找矿模式.北京:地震出版社,1-234
赵一鸣,张德全.1997.大兴安岭及其邻区铜多金属矿床成矿规律与远景评价.北京:地震出版社,1-318
周新华,英基丰,张连昌,张玉涛.2009.大兴安岭晚中生代火山岩成因与古老地块物质贡献:锆石U-Pb年龄及多元同位素制约.地球科学,34(1):1-10
周振华.2011.内蒙古黄岗锡铁矿床地质与地球化学.博士学位论文.北京:中国地质科学院,1-182
朱永峰,孙世华,毛骞,赵光.2004.内蒙古锡林格勒杂岩的地球化学研究:从Rodinia聚合到古亚洲洋闭合后碰撞造山的历史记录.高校地质学报,10(3):343-355
①内蒙古自治区地质矿产局.1995.内蒙古自治区区域矿产总结.呼和浩特:内蒙古自治区地质矿产局内部科研报告,1-786
①聂凤军,江思宏,白大明,刘翼飞,路彦明.2011c.内蒙古中东部特大型银多金属矿化集中区成矿规律、找矿方向和评价技术研究成果报告.中国地质科学院矿产资源研究所内部科研报告,1-328
Blatt H and Jones RL.1975.Proportions of exposed igneous,metamorphic,and sedimentary rocks.Geological Society of AmericaBulletin,86(8):1085-1088
Chen GD.1956.Examples of“activating region”in the Chinese platformwith special reference to the“Cathaysia”problem.Acta GeologicaSinica,36(3):239-271(in Chinese with English abstract)
Chen GD.1959.The third basic tectonic unit of the crust:Diwa district.Chinese Science Bulletin,(3):94-95(in Chinese)
Chen GD,Chen JC,Wei BL,Xue JM,Liu YX,Wen SJ,Wei ZL andHu HY.1975.A brief review on the geotectonics of China.ScientiaGeologica Sinica,(3):205-219(in Chinese with Englishabstract)
Chen YJ,Zhang C,Li N,Yang YF and Deng K.2012.Geology of theMo deposits in Northeast China.Journal of Jilin University(EarthScience Edition),42(5):1223-1268(in Chinese with Englishabstract)
Chen ZG,Zhang LC,Lu BZ,Li ZL,Wu HY,Xiang P and Huang SW.2010.Geochronology and geochemistry of the Taipingchuan coppermolybdenum deposit in Inner Mongolia,and its geologicalsignificances.Acta Petrologica Sinica,26(5):1437-1449(inChinese with English abstract)
Chen ZG,Zhang LC,Wan B,Wu HY and Cleven N.2011.Geochronology and geochemistry of the Wunugetushan porphyry CuMo deposit in NE China,and their geological significance.OreGeology Reviews,43(1):92-105
Du BF,Wei JH,Wang Q,Li YJ,Liu GC,Yu HT and Liu YL.2010.Discussion on metallogenic setting and time difference betweenmagmatism and mineralization of molybdenum deposits in EastChina.Mineral Deposits,29(6):935-955(in Chinese withEnglish abstract)
Groves DI and Bierlein FP.2007.Geodynamic settings of mineral depositsystems.Journal of the Geological Society,164(1):19-30
Hao X and Xu B.1997.Sm-Nd,Rb-Sr isotopic geochronology of theXilin Gol complex,Inner Mongolia,China.Geological Review,43(1):101-105(in Chinese with English abstract)
Holdsworth RE,Handa M,Miller JA and Buick IS.2001.Continentalreactivation and reworking:An introduction.Geological Society,London,Special Publications,184(1):1-12
Hong DW,Wang SG,Xie XL and Zhang JS.2000.Genesis of positiveεNd(t)granitoids in the Da Hinggan Mts.-Mongolia orogenic beltand growth continental crust.Earth Science Frontiers,7(2):441-456(in Chinese with English abstract)
Hong DW,Wang SG,Xie XL,Zhang JS and Wang T.2003.Metallogenic province derived from mantle sources:A case study ofcentral Asian orogenic belt.Mineral Deposits,22(1):41-55(inChinese with English abstract)
Hou ZQ,Zheng YC,Yang ZM and Yang ZS.2012.Metallogenesis ofcontinental collision setting:Part I.Gangdese Cenozoic porphyry CuMo systems in Tibet.Mineral Deposits,31(4):647-670(inChinese with English abstract)
Hurley PM and Rand JR.1969.Pre-drift continental nuclei.Science,164(3885):1229-1242
Bureau of Geology and Mineral Resources of Inner Mongolia AutonomousRegion(BGMRI).1991.Regional Geology of Inner MongoliaAutonomous Region.Beijing:Geol.Pub.House,1-725(inChinese with English abstract)
Jacobsen SB.1988.Isotopic constraints on crustal growth and recycling.Earth and Planetary Science Letters,90(3):315-329
Jia PP,Wei JH,Gong QW and Zhao WL.2011.Analysis of geologicalbackground and ore-searching prospect for the copper-molybdenumdeposits in the Da Hingan Ling area.Geology and Exploration,47(2):151-162(in Chinese with English abstract)
Jiang SH,Nie FJ,Bai DM,Liu YF and Liu Y.2011.Geochronologyevidence for Indosinian mineralization in Baiyinnuoer Pb-Zn depositof Inner Mongolia.Mineral Deposits,30(5):787-798(inChinese with English abstract)
Li JY,Zhang J,Yang TN,Li YP,Sun GH,Zhu ZX and Wang LJ.2009.Crustal tectonic division and evolution of the southern part ofthe North Asian orogenic region and its adjacent areas.Journal ofJilin University(Earth Science Edition),39(4):584-605(inChinese with English abstract)
Li SL and Ouyang ZY.1998.Tectonic framework and evolution of Xing’anling-Mongolian Orogenic Belt(XMOB)and its adjacent region.Marine Geology and Quaternary Geology,18(3):45-54(inChinese with English abstract)
Liu YF,Nie FJ,Jiang SH et al.2010.The geochronology andgeochemical features of ore-hosting granite in the Aryn Nuurmolybdenum deposit,Mongolia.Acta Geoscientica Sinica,31(3):343-349(in Chinese with English abstract)
Ma XH,Chen B,Lai Y and Lu YH.2009.Petrogenesis andmineralization chronology study on the Aolunhua porphyry Modeposit,Inner Mongolia,and its geological implications.ActaPetrologica Sinica,25(11):2939-2950(in Chinese with Englishabstract)
Meng QR.2003.What drove Late Mesozoic extension of the northernChina-Mongolia tract?Tectonophysics,369(3-4):155-174
Nie FJ,Jiang SH,Zhang Y,Liu Y and Hu P.2004.Geological featuresand origin of porphyry copper deposits in China-Mongolia borderregion and its neighboring areas.Mineral Deposits,23(2):176-189(in Chinese with English abstract)
Nie FJ,Jiang SH,Zhang Y,Bai DM,Hu P,Zhao YY,Zhang WY andLiu Y.2007a.Metallogenic Studies and Prospecting Orientation inCentral and Eastern Segments along China-Mongolia.Beijing:Geol.Pub.House,1-574(in Chinese with English abstract)
Nie FJ,Zhang WY,Du AD,Jiang SH and Liu Y.2007b.Re-Os isotopicage dating of molybdenite separates from the Chaobuleng skarn ironpolymetallic deposit,Dong Ujimqin banner,Inner Mongolia.ActaGeoscientica Sinica,28(4):315-323(in Chinese with Englishabstract)
Nie FJ,Jiang SH,Bai DM,Hou WR and Liu YF.2010a.Types andtemporal-spatial distribution of metallic deposits in southern Mongoliaand its neighboring areas.Acta Geoscientica Sinica,31(3):267-288(in Chinese with English abstract)
Nie FJ,Hu P,Jiang SH and Liu YF.2010b.Geological features,geochronology and origin of the tungsten and tungsten(molybdenum)deposits in the Shamai-Yuguzer mineralizationconcentrated camp along the Sino-Mongolian border.ActaGeoscientica Sinica,31(3):383-394(in Chinese with Englishabstract)
Nie FJ and Jiang SH.2011.Geological setting and origin of Mo-W-Cudeposits in the Honggor-Shamai district,Inner Mongolia,NorthChina.Resource Geology,61(4):344-355
Nie FJ,Sun ZJ,Li C,Liu YF,LüKP,Zhang K and Liu Y.2011a.ReOs isotopic dating of molybdenite separates from Chalukou porphyryMo polymetallic deposit in Heilongjiang Province.Mineral Deposits,30(5):828-836(in Chinese with English abstract)
Nie FJ,Zhang K,Liu YF,Jiang SH,Liu Y and Liu Y.2011b.Indosinian magamtic activity and molybdenum,gold mineralizationalong the northern margin of North China craton and adjacent area.Journal of Jilin University(Earth Science Edition),41(6):1651-1666(in Chinese with English abstract)
Nie FJ,Sun ZJ,Liu YF,LüKP,Zhao YA and Cao Y.2013.Mesozoicmultiple magmatic activities and molybdenum mineralization in theChalukou ore district,Da Hinggan mountains.Geology in China,40(1):273-286(in Chinese with English abstract)
Nie XL and Hou WR.2010.The discovery of the Diyanqinamu large-sizeMo-Ag deposit,Inner Mongolia,and its geological significance.ActaGeoscientica Sinica,31(3):469-472(in Chinese with Englishabstract)
Pei RF.1995.Mineral Deposit Models of China.Beijing:GeologicalPublishing House,331-336(in Chinese)
Pirajno F,Ernst RE,Borisenko AS et al.2009.Intraplate magmatism incentral Asia and China and associated metallogeny.Ore GeologyReviews,35(2):114-136
Ren JS,Wang ZX,Chen BW,Jiang CF,Nie BG,Li JY,Xie GL,HeZJ and Liu ZG.1999.The Tectonics of China from A Global View:A Guide to Tectonic Map of China and Adjacent Region.Beijing:Geological Publishing House,1-32
Richards JP.2009.Post subduction porphyry Cu-Au and epithermal Audeposits:Products of remelting of subduction-modified lithosphere.Geology,37(3):247-250
Robert F,Brommecker R,Bourne BT,Dobak PJ,McEwan CJ,RoweRR and Zhou X.2007.Models and exploration methods for majorgold deposit types.In:Milkereit B(ed.).Proceedings ofExploration 07:Fifth Decennial International Conference on MineralExploration,691-711
Shen GY.2008.Geological characteristics and prospecting direction ofHaolihao copper-molybdenum deposit in Arhorqin,Inner Mongolia.Geology and Resources,17(4):273-277(in Chinese with Englishabstract)
Sun JG,Zhang Y,Xing SW,Zhao KQ,Zhang ZJ,Bai LA,Ma YB andLiu YS.2012.Genetic types,ore-forming age and geodynamicsetting of endogenic molybdenum deposits in the eastern edge ofXing-Meng orogenic belt.Acta Petrologica Sinica,28(4):1317-1332(in Chinese with English abstract)
Sun LX,Ren BF,Zhao FQ,Gu YC,Li YF and Liu H.2013a.ZirconU-Pb dating and Hf isotopic compositions of the mesoporterozoicgranitic gneiss in Xilinhot block,Inner Mongolia.GeologicalBulletin of China,32(2-3):327-340(in Chinese with Englishabstract)
Sun LX,Ren BF,Zhao FQ,Ji SP and Geng JZ.2013b.LatePaleoproterozoic magmatic records in the Eerguna massif:Evidencesfrom the zircon U-Pb dating of granitic gneisses.Geological Bulletinof China,32(2-3):341-352(in Chinese with English abstract)
Taylor RG.1979.Geology of Tin Deposits-Developments in EconomicGeology.Oxford,Amsterdam and New York:Elsevier Science Ltd,1-544
Vervoort JD and Blichert-Toft J.1999.Evolution of the depleted mantle:Hf isotope evidence from juvenile rocks through time.Geochimica etCosmochimica Acta,63(3-4):533-556
Wang F,Zhou XH,Zhang LC et al.2006.Late mesozoic volcanism inthe Great Xing’an Range(NE China):Timing and implications forthe dynamic setting of NE Asia.Earth and Planetary Science Letters,251(1-2):179-198
Wang JB,Wang YW,Wang LJ and Uemoto T.2001.Tin-polymetallicmineralization in the southern part of the Da Hinggan Mountains,China.Resource Geology,51(4):283-291
Wang MY and He L.2013.Re-Os dating of molybdenites from ChamuhanW-Mo deposit,Inner Mongolia and its geological implications.Geotectonica et Metallogenia,37(1):49-56(in Chinese withEnglish abstract)
Wang YW,Wang JB,Uemoto T and Wang LJ.2001.Geology andmineralization at the Dajing tin-polymetallic ore deposit,InnerMongolia,China.Resource Geology,51(4):307-320
Wu G,Chen YC,Chen YJ and Zeng QT.2012.Zircon U-Pb ages of themetamorphic supracrustal rocks of the Xinghuadukou Group andgranitic complexes in the Argun massif of the northern Great HingganRange,NE China,and their tectonic implications.Journal of AsianEarth Sciences,49:214-233
Xiang AP,She HQ,Guan JD,Kang YJ,Han ZG,Li JW,Yang YC andGuo ZJ.2014.Study on the metallogenic and diagenetic age ofHonghuaerji tungsten polymetallic deposit in Inner Mongolia.MineralDeposits,33(2):428-439(in Chinese with English abstract)
Xu B,Chen B and Shao JA.1996.Sm-Nd and Rb-Sr geochronologicalstudies on Xilinguole complex.Chinese Science Bulletin,41(2):153-155(in Chinese)
Xu ZG.1997.Tectonic evolution and its controlling factors on the oreforming processes of the in the Da Hinggan mountains and itsadjacent regions.In:Zhao YM and Zhang DQ(eds.).Metallogenyand Prospective Evaluation of Copper-polymetallic Deposits in the DaHinggan Mountains and Its Adjacent Regions.Beijing:SeismologicalPress,1-21(in Chinese)
Xue J,Nie FJ,Dai TG,Peng ES and Liu YF.2010.Re-Os isotopicdating of molybdenite from the Aryn nuur Mo deposit in Mongolia andits geological implications.Acta Geoscientica Sinica,31(3):350-356(in Chinese with English abstract)
Yan C,Sun Y,Lai Y and Ma XH.2011.LA-ICP-MS zircon U-Pb andmolybdenite Re-Os isotope ages and metallogenic geodynamic settingof Banlashan Mo deposit,Inner Mongolia.Mineral Deposits,30(4):616-634(in Chinese with English abstract)
Yang YC.2010.Metallogenic studies and prospecting orientation onDeerbugan metallogenic zone and adjacent area.Post-DoctorResearch Report.Beijing:Chinese Academy of Geological Sciences,1-148(in Chinese with English summary)
Zhang K,Nie FJ,Hou WR,Li C and Liu Y.2012.Re-Os isotopic agedating of molybdenite separates from Hashitu Mo deposit in LinxiCounty of Inner Mongolia and its geological significance.MineralDeposits,31(1):129-138(in Chinese with English abstract)
Zhang LC,Wu HY,Xiang P,Zhang XJ,Chen ZG and Wan B.2010.Ore-forming processes and mineralization of complex tectonic systemduring the Mesozoic:A case from Xilamulun Cu-Mo metallogenicbelt.Acta Petrologica Sinica,26(5):1351-1362(in Chinesewith English abstract)
Zhao YM,Wang DW,Zhang DQ,Fu XZ,Bao XP,Li HN and Ai YF.1994.Ore-controlling Factors and Ore-prospecting Models forCopperpolymetallic Ore Deposits in Southeastern Inner Mongolia.Beijing:Seismological Publishing House,1-234(in Chinese)
Zhao YM and Zhang DQ.1997.Metallogeny and Prospective Evaluationof Copper-polymetallic Deposits in the Da Hinggan Mountains and ItsAdjacent Regions.Beijing:Seismological Press,1-318(inChinese)
Zhou XH,Ying JF,Zhang LC and Zhang YT.2009.The petrogenesis oflate Mesozoic volcanic rock and the contributions from ancient microcontinents:Constraints from the zircon U-Pb dating and Sr-Nd-Pb-Hfisotopic systematics.Earth Science,34(1):1-10(in Chinesewith English abstract)
Zhou ZH.2011.Geology and geochemistry of Huanggang Sn-Fe deposit,Inner Mongolia.Ph.D.Dissertation.Beijing:Chinese Academy ofGeological Sciences,1-182(in Chinese with English summary)
Zhu YF,Sun SH,Mao Q and Zhao G.2004.Geochemistry of theXilingele complex,Inner Mongolia:A historic record from rodiniaaccretion to continental collision after closure of the Paleo-AsianOcean.Geological Journal of China Universities,10(3):343-355(in Chinese with English abstract)
别洛乌索夫.1955.大地构造的基本问题.地质学报,35(3):177-189
陈国达.1956.中国地台“活化区”的实例,并着重讨论“华夏古陆”问题.地质学报,36(3):239-271
陈国达.1959.地壳的第三基本构造单元———地洼区.科学通报,(3):94-95
陈国达,陈家超,魏柏林,薛佳谋,刘以宣,文善继,魏洲龄,胡火炎.1975.中国大地构造简述.地质科学,(3):205-219
陈衍景,张成,李诺,杨永飞,邓轲.2012.中国东北钼矿床地质.吉林大学学报(地球科学版),42(5):1223-1268
陈志广,张连昌,卢百志,李占龙,吴华英,相鹏,黄世武.2010.内蒙古太平川铜钼矿成矿斑岩时代、地球化学及地质意义.岩石学报,26(5):1437-1449
杜保峰,魏俊浩,王启,李艳军,刘国春,于海涛,刘永利.2010.中国东部钼矿成矿背景与成岩-成矿时差讨论.矿床地质,29(6):935-955
郝旭,徐备.1997.内蒙古锡林浩特锡林郭勒杂岩的原岩年代和变质年代.地质评论,43(1):101-105
洪大卫,王式光,谢锡林,张季生.2000.兴蒙造山带正εNd(t)值花岗岩的成因和大陆地壳生长.地学前缘,7(2):441-456
洪大卫,王式光,谢锡林,张季生,王涛.2003.试析地幔来源物质成矿域———以中亚造山带为例.矿床地质,22(1):41-55
侯增谦,郑远川,杨志明,杨竹森.2012.大陆碰撞成矿作用:I.冈底斯新生代斑岩成矿系统.矿床地质,31(4):647-670
贾盼盼,魏俊浩,巩庆伟,赵万莉.2011.大兴安岭地区铜钼矿床成矿区带背景及找矿前景分析.地质与勘探,47(2):151-162
江思宏,聂凤军,白大明,刘翼飞,刘妍.2011.内蒙古白音诺尔铅锌矿床印支期成矿的年代学证据.矿床地质,30(5):787-798
李锦轶,张进,杨天南,李亚萍,孙桂华,朱志新,王励嘉.2009.北亚造山区南部及其毗邻地区地壳构造分区与构造演化.吉林大学学报(地球科学版),39(4):584-605
李双林,欧阳自远.1998.兴蒙造山带及邻区的构造格局与构造演化.海洋地质与第四纪地质,18(3):45-54
刘翼飞,聂凤军,江思宏,薛静,侯万荣,云飞.2010.蒙古国阿林诺尔钼矿床赋矿花岗岩年代学及地球化学特征.地球学报,31(3):343-349
马星华,陈斌,赖勇,鲁颖淮.2009.内蒙古敖仑花斑岩钼矿床成岩成矿年代学及地质意义.岩石学报,25(11):2939-2950
内蒙古自治区地质矿产局.1991.内蒙古自治区区域地质志.北京:地质出版社,1-725
聂凤军,江思宏,张义,刘妍,胡朋.2004.中蒙边境及邻区斑岩型铜矿床地质特征及成因.矿床地质,23(2):176-189
聂凤军,江思宏,张义,白大明,胡朋,赵元艺,张万益,刘妍.2007a.中蒙边境中东段金属矿床成矿规律和找矿方向.北京:地质出版社,1-574
聂凤军,张万益,杜安道,江思宏,刘妍.2007b.内蒙古朝不楞矽卡岩型铁多金属矿床辉钼矿铼-锇同位素年龄及地质意义.地球学报,28(4):315-323
聂凤军,江思宏,白大明,侯万荣,刘翼飞.2010a.蒙古国南部及邻区金属矿床类型及其时空分布特征.地球学报,31(3):267-288
聂凤军,胡朋,江思宏,刘翼飞.2010b.中蒙边境沙麦-玉古兹尔地区钨和钨(钼)矿床地质特征,形成时代和成因机理.地球学报,31(3):383-394
聂凤军,孙振江,李超,刘翼飞,吕克鹏,张可,刘勇.2011a.黑龙江岔路口钼多金属矿床辉钼矿铼-锇同位素年龄及地质意义.矿床地质,30(5):828-836
聂凤军,张可,刘翼飞,江思宏,刘勇,刘妍.2011b.华北克拉通北缘及邻区印支期岩浆活动与钼和金成矿作用.吉林大学学报(地球科学版),41(6):1651-1666
聂凤军,孙振江,刘翼飞,吕克鹏,赵宇安,曹毅.2013.大兴安岭岔路口矿区中生代多期岩浆活动与钼成矿作用.中国地质,40(1):273-286
聂秀兰,侯万荣.2010.内蒙古迪彦钦阿木大型钼-银矿床的发现及地质意义.地球学报,31(3):469-472
裴荣富.1995.中国矿床模式.北京:地质出版社,331-336
沈光银.2008.内蒙古阿鲁科尔沁旗好力宝铜钼矿床地质特征及找矿方向.地质与资源,17(4):273-277
孙景贵,张勇,邢树文,赵克强,张增杰,白令安,马玉波,刘勇胜.2012.兴蒙造山带东缘内生钼矿床的成因类型、成矿年代及成矿动力学背景.岩石学报,28(4):1317-1332
孙立新,任邦方,赵凤清,谷永昌,李艳峰,刘卉.2013a.内蒙古锡林浩特地块中元古代花岗片麻岩的锆石U-Pb年龄和Hf同位素特征.地质通报,32(2-3):327-340
孙立新,任邦方,赵凤清,冀世平,耿建珍.2013b.内蒙古额尔古纳地块古元古代末期的岩浆记录-来自花岗片麻岩的锆石U-Pb年龄证据.地质通报,32(2-3):341-352
王明艳,何玲.2013.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.大地构造与成矿学,37(1):49-56
向安平,佘宏全,关继东,康永建,韩增光,李进文,杨郧城,郭志军.2014.内蒙古红花尔基钨多金属矿成岩成矿年代学研究.矿床地质,33(2):428-439
徐备,陈斌,邵济安.1996.内蒙古锡林郭勒杂岩Sm-Nd,Rb-Sr同位素年代研究.科学通报,41(2):153-155
徐志刚.1997.大兴安岭及其邻区构造演化及控矿作用.见:赵一鸣,张德全主编.大兴安岭及其邻区铜多金属矿床成矿规律与远景评价.北京:地震出版社,1-21
薛静,聂凤军,戴塔根,彭恩生,刘翼飞.2010.蒙古国阿林诺尔钼矿床辉钼矿Re-Os同位素年龄及地质意义.地球学报,31(3):350-356
闫聪,孙艺,赖勇,马星华.2011.内蒙古半拉山钼矿LA-ICP-MS锆石U-Pb与辉钼矿Re-Os年龄及其成矿动力学背景.矿床地质,30(4):616-634
杨郧城.2010.得尔布干成矿带及邻区成矿规律与找矿方向研究.博士后研究工作报告.北京:中国地质科学院,1-148
张可,聂凤军,侯万荣,李超,刘勇,2012.内蒙古林西县哈什吐钼矿床辉钼矿铼-锇年龄及其地质意义.矿床地质,31(1):129-138
张连昌,吴华英,相鹏,张晓静,陈志广,万博.2010.中生代复杂构造体系的成矿过程与成矿作用:以华北大陆北缘西拉木伦钼铜多金属成矿带为例.岩石学报,26(5):1351-1362
赵一鸣,王大畏,张德全,傅先政,鲍修坡,李鹤年,艾永富.1994.内蒙古东南部铜多金属成矿地质条件及找矿模式.北京:地震出版社,1-234
赵一鸣,张德全.1997.大兴安岭及其邻区铜多金属矿床成矿规律与远景评价.北京:地震出版社,1-318
周新华,英基丰,张连昌,张玉涛.2009.大兴安岭晚中生代火山岩成因与古老地块物质贡献:锆石U-Pb年龄及多元同位素制约.地球科学,34(1):1-10
周振华.2011.内蒙古黄岗锡铁矿床地质与地球化学.博士学位论文.北京:中国地质科学院,1-182
朱永峰,孙世华,毛骞,赵光.2004.内蒙古锡林格勒杂岩的地球化学研究:从Rodinia聚合到古亚洲洋闭合后碰撞造山的历史记录.高校地质学报,10(3):343-355
①内蒙古自治区地质矿产局.1995.内蒙古自治区区域矿产总结.呼和浩特:内蒙古自治区地质矿产局内部科研报告,1-786
①聂凤军,江思宏,白大明,刘翼飞,路彦明.2011c.内蒙古中东部特大型银多金属矿化集中区成矿规律、找矿方向和评价技术研究成果报告.中国地质科学院矿产资源研究所内部科研报告,1-328