黑龙江小兴安岭—张广才岭成矿带成矿系列及找矿远景评价
|
摘要
小兴安岭—张广才岭成矿带位于中亚—兴蒙造山带东段,西伯利亚地块、华北地块和太平洋板块的交汇区域,是经古亚洲洋构造域与滨太平洋构造域强烈叠加而成的复合造山带,具有独特构造演化背景。在两大构造域转换时期,该区发生大规模成岩成矿作用。
首先,在成矿相关岩浆岩岩石学和成岩成矿年代学研究基础上,系统划分出矿床成矿系列,并对成矿系列地质地球化学和流体包裹体进行研究,建立了成矿动力学模型。(1)燕山早期与中酸性花岗岩有关的多金属矿床成矿系列(Ⅰ)：包括矽卡岩型、斑岩型和热液脉型及其复合类型矿床。获得相关花岗岩类岩石锆石U—Pb年龄和辉钼矿Re-Os年龄分别为195-175Ma和180-175Ma,结合前人相关研究结果,认为其成岩成矿作用发生于晚三叠世—早侏罗世,其中成岩大致始于T3,成矿于J1,成岩成矿大致结束于172Ma。与成矿相关的花岗岩属钙碱性—高钾钙碱性系列,具有Ⅰ型和A型花岗岩特征,成岩成矿发生于造山期后岩石圈伸展减薄环境。成岩成矿物质主要来自地壳,成矿流体主要来自岩浆,部分来自大气降水。氧化物阶段成矿温度大致为380～500℃,硫化物阶段成矿温度大致为250～360℃,推测的成矿深度为2-3km。包裹体特征显示,在成矿过程中可能发生过不同流体相互混合和流体沸腾作用。(2)燕山晚期与火山作用有关的金银、铅锌矿床成矿系列(Ⅱ)：以浅成低温热液型金矿床为主。获得与之相关流纹岩锆石U-Pb年龄约为110Ma,辉绿玢岩角闪石Ar-Ar年龄约为100Ma,结合前人相关研究结果,认为该成矿系列成岩成矿作用发生于120～100Ma,其中成岩始于120Ma,金成矿年龄为110～105Ma,金成矿稍晚于成岩,辉绿玢岩及与之相关的改造型铅锌矿形成最晚。该成矿系列成岩成矿作用发生于太平洋板块俯冲体制下的地壳加厚构造环境,成岩成矿物质主要来自下地壳或上地幔,成矿流体主要来自大气降水,部分来自岩浆。浅成低温热液型金矿床成矿温度为150～280℃,成矿流体盐度低,成矿深度约为1.2～2.0km。
最后,在总结成矿规律基础上,建立了预测模型,并采用综合信息成矿预测方法,对成矿远景进行评价。成矿系列(Ⅰ)分布于早中生代花岗岩带,成矿具同源性、共生性、阶段性、分带性、叠加性、过渡性和互补性。早期为矽卡岩型铁钨锡成矿阶段,晚期为斑岩型钼矿和热液型铜铅锌矿成矿阶段。斑岩型钼矿、矽卡岩型多金属矿和热液脉型铜铅锌矿分别产于岩体内、接触带和外接触带。成矿系列(Ⅱ)分布于晚中生代火山活动带,受裂隙—中心式火山机构控制。共圈定8个成矿远景区,并提出找矿方向。
The Lasser Xing'an Range-Zhangguangcai Range metallogenic belt is composite orogen belt superposed by Paleoasia oceanic tectonic domain and circle Pacific tectonic domian, lying in the intersection area among east section of Central Asian-Mongolian-Hinggan orogenic belt and Siberian,North China blocks. In the two tectonic domain transformation period, large-scale mineralization and diagenesis occured.
On the basis of study magmatic petrology and diagenesis mineralization chronology, to the division of metallogenic series of ore deposits, to the study of geology and geochemistry and fluid inclusion, establishing the model of metallogenic dynamics.(1) The metallogenic series of intermediate-acid granitoids polymetallic deposit in early Yanshan Period(I):including skarn type, porohyry type, hydrothermal vein type, compound deposit. The zircon U-Pb age of195-175Ma and molybdenite Re-Os age of180～175Ma was obtained from granite, indicating that the suite formed in the Late Triassic-Early Jurassic Epoch, diagenesis in Late Triassic and mineralization in Late Triassic, ended in172Ma. Granitoids related to the mineralization belong to calc-alkaline series to high kalium calc alkalic series, charactered by I and A type, diagenesis and mineralization occurred after orogenic period and lithospheric extension and thinning. Materials source of diagenesis and mineralization comes from crust and the ore-forming fluid is meanly from and magmatic and atmosphere precipitation. The metallogenic temperature of oxide is380～500℃, sulfide250～360℃, depth of2～3km. Fluid inclusion studies that different fluid mixing and boiling during the metallogenic process.(2) In the late Yanshanian, related with volcanism, Au-Ag-Pb-Zn deposit series (II):The epithermal gold deposit. Rhyolite zircon U-Pb age of110Ma and sillite hornblende Ar-Ar age of100Ma, was obtained, indicating that the formed in the120～100Ma, diagenesis in120Ma and gold mineralization in110～105Ma, ended in sillite and releated lead-zinc mine. Diagenesis and mineralization of the metallogenetic series occurred in tectonic environment of the subduction of pacific plate lead to crust thickening, material source of diagenesis and mineralization is from the lower crust or upper mantle and ore-forming fluid is derived meanly from atmospheric precipitation and partly magmatic. The ore-forming temperature of the epithermal gold deposit is150～280℃. The ore forming fluids had very low salinity, depth of1.2～2.0km.
Summarizing metallogenic regularities, establishing prediction modles, adopting comprehensive information metallogenic prediction method, this paper evaluates ore-forming prospects. The metallogenetic series (Ⅰ) distributed in granite belt of the early Mesozoic, the character of metallogenic symbiosis stage, homology, superpositon and transitivity. Metallogenic stages of skarn type iron tungsten tin occurred earlier, and late porphyry molybdenum deposit and hydrothermal type copper lead and zinc deposit. Porphyry molybdenum deposit, skarn type polymetallic deposits and hydrothermal type copper lead and zinc deposit come from internal zone, contact zone outer contact zones respectively. The metallogenetic series (Ⅱ) distributed in active belt in the late Mesozoic, controlled by fissure-central volcanic types. The paper outlines8metallogenic prospects and proposes direction of further exploration.
首先,在成矿相关岩浆岩岩石学和成岩成矿年代学研究基础上,系统划分出矿床成矿系列,并对成矿系列地质地球化学和流体包裹体进行研究,建立了成矿动力学模型。(1)燕山早期与中酸性花岗岩有关的多金属矿床成矿系列(Ⅰ)：包括矽卡岩型、斑岩型和热液脉型及其复合类型矿床。获得相关花岗岩类岩石锆石U—Pb年龄和辉钼矿Re-Os年龄分别为195-175Ma和180-175Ma,结合前人相关研究结果,认为其成岩成矿作用发生于晚三叠世—早侏罗世,其中成岩大致始于T3,成矿于J1,成岩成矿大致结束于172Ma。与成矿相关的花岗岩属钙碱性—高钾钙碱性系列,具有Ⅰ型和A型花岗岩特征,成岩成矿发生于造山期后岩石圈伸展减薄环境。成岩成矿物质主要来自地壳,成矿流体主要来自岩浆,部分来自大气降水。氧化物阶段成矿温度大致为380～500℃,硫化物阶段成矿温度大致为250～360℃,推测的成矿深度为2-3km。包裹体特征显示,在成矿过程中可能发生过不同流体相互混合和流体沸腾作用。(2)燕山晚期与火山作用有关的金银、铅锌矿床成矿系列(Ⅱ)：以浅成低温热液型金矿床为主。获得与之相关流纹岩锆石U-Pb年龄约为110Ma,辉绿玢岩角闪石Ar-Ar年龄约为100Ma,结合前人相关研究结果,认为该成矿系列成岩成矿作用发生于120～100Ma,其中成岩始于120Ma,金成矿年龄为110～105Ma,金成矿稍晚于成岩,辉绿玢岩及与之相关的改造型铅锌矿形成最晚。该成矿系列成岩成矿作用发生于太平洋板块俯冲体制下的地壳加厚构造环境,成岩成矿物质主要来自下地壳或上地幔,成矿流体主要来自大气降水,部分来自岩浆。浅成低温热液型金矿床成矿温度为150～280℃,成矿流体盐度低,成矿深度约为1.2～2.0km。
最后,在总结成矿规律基础上,建立了预测模型,并采用综合信息成矿预测方法,对成矿远景进行评价。成矿系列(Ⅰ)分布于早中生代花岗岩带,成矿具同源性、共生性、阶段性、分带性、叠加性、过渡性和互补性。早期为矽卡岩型铁钨锡成矿阶段,晚期为斑岩型钼矿和热液型铜铅锌矿成矿阶段。斑岩型钼矿、矽卡岩型多金属矿和热液脉型铜铅锌矿分别产于岩体内、接触带和外接触带。成矿系列(Ⅱ)分布于晚中生代火山活动带,受裂隙—中心式火山机构控制。共圈定8个成矿远景区,并提出找矿方向。
The Lasser Xing'an Range-Zhangguangcai Range metallogenic belt is composite orogen belt superposed by Paleoasia oceanic tectonic domain and circle Pacific tectonic domian, lying in the intersection area among east section of Central Asian-Mongolian-Hinggan orogenic belt and Siberian,North China blocks. In the two tectonic domain transformation period, large-scale mineralization and diagenesis occured.
On the basis of study magmatic petrology and diagenesis mineralization chronology, to the division of metallogenic series of ore deposits, to the study of geology and geochemistry and fluid inclusion, establishing the model of metallogenic dynamics.(1) The metallogenic series of intermediate-acid granitoids polymetallic deposit in early Yanshan Period(I):including skarn type, porohyry type, hydrothermal vein type, compound deposit. The zircon U-Pb age of195-175Ma and molybdenite Re-Os age of180～175Ma was obtained from granite, indicating that the suite formed in the Late Triassic-Early Jurassic Epoch, diagenesis in Late Triassic and mineralization in Late Triassic, ended in172Ma. Granitoids related to the mineralization belong to calc-alkaline series to high kalium calc alkalic series, charactered by I and A type, diagenesis and mineralization occurred after orogenic period and lithospheric extension and thinning. Materials source of diagenesis and mineralization comes from crust and the ore-forming fluid is meanly from and magmatic and atmosphere precipitation. The metallogenic temperature of oxide is380～500℃, sulfide250～360℃, depth of2～3km. Fluid inclusion studies that different fluid mixing and boiling during the metallogenic process.(2) In the late Yanshanian, related with volcanism, Au-Ag-Pb-Zn deposit series (II):The epithermal gold deposit. Rhyolite zircon U-Pb age of110Ma and sillite hornblende Ar-Ar age of100Ma, was obtained, indicating that the formed in the120～100Ma, diagenesis in120Ma and gold mineralization in110～105Ma, ended in sillite and releated lead-zinc mine. Diagenesis and mineralization of the metallogenetic series occurred in tectonic environment of the subduction of pacific plate lead to crust thickening, material source of diagenesis and mineralization is from the lower crust or upper mantle and ore-forming fluid is derived meanly from atmospheric precipitation and partly magmatic. The ore-forming temperature of the epithermal gold deposit is150～280℃. The ore forming fluids had very low salinity, depth of1.2～2.0km.
Summarizing metallogenic regularities, establishing prediction modles, adopting comprehensive information metallogenic prediction method, this paper evaluates ore-forming prospects. The metallogenetic series (Ⅰ) distributed in granite belt of the early Mesozoic, the character of metallogenic symbiosis stage, homology, superpositon and transitivity. Metallogenic stages of skarn type iron tungsten tin occurred earlier, and late porphyry molybdenum deposit and hydrothermal type copper lead and zinc deposit. Porphyry molybdenum deposit, skarn type polymetallic deposits and hydrothermal type copper lead and zinc deposit come from internal zone, contact zone outer contact zones respectively. The metallogenetic series (Ⅱ) distributed in active belt in the late Mesozoic, controlled by fissure-central volcanic types. The paper outlines8metallogenic prospects and proposes direction of further exploration.
引文
Abramovich I I, Klushin I G..Geodynamics and Metallogeny of Folded Belts. New Delhi:Oxford & IBH Pub.Co.Pvt. Ltd.,1990
Alok Porwal,Emmanuel John M Carranza,Martin Hale. A hybridfuzzy wights-of-evidence model for mineral potential mapping. Natural Resources Research,2006,15(1):1-14
Badham J P N. Strike-sliporogens-an expantion for the Hereynides. Geol. Soc. London,1982,139:493-504
Barley M E.,Groves D I. Supercontinent cycles and the distribution of metal deposits through time. Geology,1992,20:291-294
Barnes H L. Energetics of Hydrothermal Ore Deposits in Frontiers in Geochemistry:Organic, Solution and Ore Deposit Geochemistry. Columbia:Bellwether Publishing,Ltd,2002,184-190
Bilibin Y A. Metallogenic Provinces and Metallogenic Epochs. New York:Queenscoll Flushing,1955,35
Bonham,Carter G F. Geographic Information Systems for Geoscientist:Modelling with GIS. Oxford:Linacre House,1994:317-337
Chen J P, Wang G W, Hou C B.Quantitative Prediction and Evaluation of Mineral Resources Based on GIS:A Case Study in Sanjiang Region,Southwestern China. Natural Resources Research,2005,14(4):285-294
Chen Y J.Mineralization during collisional orogenesis and its control of the distribution of gold deposits in Junggar Mountains, Xinjiang, China. Acta Geologica Sinica,1997,71(1):69-79
Christensen J N, Halliday A N, Leigh K E, et al. Direct dating of sulfides by Rb-Sr:Acritical test using the Polaris Mississippi Valley-type Zn-Pb deposit. Geochimica. et Cosmochimica. Acta,1995,59:5191-5197
Condie K C. Mantle plume and their record in earth history. London:Cambridge University Press,2001
Corbett G J, Leach T M. Southwest Pacific Rim gold-copper systems:structure, alteration and mineralization. Society of Economic Geologists Special Publication,1998,6:1-240
Cline J S. Bodnar R J. Can economic porphyry copper mineralization be generated by a typical calc-alkaline melt. Geophys Res,1991,96:8113-8126
De Grave J, Buslov M M and Van den haute P. Distante ects of India-Eurasia convergence and Mesozoic intracontinental deformation in Central Asia:Constraints from apatite? ssion-track thermochronoloy.Journal of Asian Earth Seiences,2007,29:188-204
Fang W X, Zhang G W, Lu J Y, et al. Complexity and geodynamics of ore-accumulating basin in the Qinling orogenic belt, China. Act a Geo Sinica,2000,74(3):458-465
Gill J B. Orogenie Andesites and Piate Tectonies. Berlin:Springer-Verlag,1981,358-360
Goldfarb R J, Philips G N, Nokleberg W J. Tectonic setting of synorogenic gold deposits of the Pacific Rim. Ore Geology Reviews,1998,13:185-218
Goldfarb R J, Geoves D I,Gardoll S. Orogenic gold and geologictime:A global synthesis. Ore Geology Reviews,2001,18:1-75
Groves D I, Goldfarb R J, Gebre-Maiam M,et al. Orogenic gold deposits:A proposed classification in the context of their crustal distribution and relationship to other gold deposit types. Ore Geology Reviews, 1998,13:7-27
Groves D I, Goldfarb R J, Knox-Robinson C M, et al. Late kinematic timing of orogenic gold deposits and significance for computer-based exploration techniques with emphasison the Yilgarn Block, Weatern Australia. Ore Geology Reviews,2000,17:1-38
Grove D I, Condie K C, Goldfarb R J, Hronsky J M A, Vielreicher R M. Secular changes in golobal tectonic processes and their influence on the temporal distribution of gold-bearing mineral deposits. Economic Geology 100th Anniversary Volume,2005,203-224
Groves D I, Bierlein F P. Geodynamic settings of mineral deposit systems. Journal of the Geological Society, London,2007,164:19-30
Hall, D.L., S.M. Sterner and R.J. Bodnar. Freezing point depression of NaCl-KCl-H2O solutions. Econ.Geol. 1988,83:197-202
Hartmann L A, Delgado I M. Cratons and orogenic belts of the Brazilian shield and their contained gold deposits. Mineralium Deposita,2001,36(34):207-217
Hedenquist J W, Lowenstern J B. The role of magmas in the formation of hydrothermal ore deposits. Nature,1994,370(4):519-527
Henley R W, Ellis A J.Geothermal systems ancient and modern:a geochemical review.Earth Sci Rev, 1983,19:1-50
Huang D H, Du A D, Wu C Y, et al. Metallochronology of molybdenum (-copper) deposits in the north China platform:Re-Os age of molybdenite and its geological significance. Mineral Deposits,1996,15 (4):365-372
Hu Z C, Liu Y S, Gao S, et al. A local aerosol extraction strategy for the determination of the aerosol composition in LA-ICP-MS. Journal of Analytical Atomic Spectrometry,2008,23:1192-1203
Hugh R.R. Using geochemical data:Evaluation, Presentation, UK:Interpretation. Pearson Education Limited.1993
Kerrich R, Goldfarb R,Groves D, Garwin S. The characteristics, origins,and geodynamic settings of supergiant gold metallogenic provinces. Science in China,2001,43:1-68
Kerrich R, Goldfarb R J, Richards J. Metallogenic provinces in an evolving geodynamic framework. Economic Geology 100th Anniversary Volume,2005,1097-1136
Leach D L, Sangster D F, Kelley K D, Large R R, Garven G, Allen C R, Gatzmer J.Wallters S. Sediment-Hosted Lead-Zink Deposit:A Global Perspective. Economic Geology 100th Anniversary Volume,2005, 561-607
Ludwig, K R. ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel. Berkeley:Berkeley Geochronology Center, California,2003
Mao J W, Zhang Z H. Re-Os Isotopic dating of molybdenites in the Xiaoliugou W(Mo) deposit in the Northern Qilian Mountains and its geological significance. Geochimica et Cosmochimica Acta,1999,63(11/12):1815-1818
Mitchell A H G, Garson M S. Mineral Deposits and Global Tectonic Settings. London:Academic Press,1981, 1-405
Nakai S, Halliday A N,Kesler S E, et al. Rb-Sr dating of sphalerite and genesis of MVT deposits. Nature, 1990,346:354-357
Nakai S, Halliday A N, Kesler S E, et al. Rb-Sr dating of sphalerites from Mississippi Valley-type(MVT) ore deposits. Geochimica. et Cosmochimica. Acta,1993,57:417-427
Sawkins J. Metal Deposits in Relation to Plate Tectonic. Berlin:Springer-Verlag,1984,283-294
Sheppard S M F, Nielsen R L, Taylor H P. Hydrogen and oxygen isotope ratios in minerals from porphyry copper deposits. Econ Geol,1971,66:515-542
Sillitoe RH, Perello J. Andean copper province:tectonomagmatic settings. Economic Geology 100th Annivers ary volume,2005,845-890
Sillitoe RH, Mortensen JK. Longevity of porphyry copper formation at Quellaveco, Peru. Economic Geology, 2010a,105:1157-1162
Sillitoe RH. Porphyry copper systems. Economic Geology,2010b,105:2-41
Singer D A. Basic concepts in three-part quantitative assessments of undiscovered mineral resources. Nonrenewable Resources,1993,2(2):69-81
Sobel E R,Chen J and Heermance R V. Late Oligocene-Early Miocene initiation of shortening in the Southwestern Chinese Tian Shan:Implications for Neogene shortening rate variations.Earth and Planetary Seience Letters,2006,247:70-81
Stein H J, Markey R J, Morgan J W, Du A, Sun Y. Highly precise and accurate Re-Os ages for molybdenum from the East Qinling molybdenum belt, Shanxi Province, China. Economic Geology.1997,98:175-180
Steiger, R.H. and Jager, E. Subcommission on geochronology:convention on the use of decay constants in geo-and cosmochronology. Earth Planet. Sci. Lett.,1977,36:359-362
Sterner S M, et al. Synthetic fluid inclusions:V. Solubility relations in the system NaCl-KCl-H2O under vapor-aaturated eonditions. Geochim.Cosmochim. Acta,1988,52:989-1005.
Titley S R, Beane R E. Porphyry copper deposits Part I.Geologic settings, petrology and tectogenesis. Econ Geol,1981,75:214-269
Wu F Y, Jahn B M, Wilde S A and D Y. Phanerozoic crustal growth:U-Pb and Sr-Nd isotoie evidence From the granites in northeastern China.TeetonoPhysies,2000,328:89-113
Wu F Y. Sun D Y, Li H M, et al. A-type ganites in northeastern China:age and geoehemical constraints on their petrogenesis. Chemical Geology,2002,187:143-173
Wu F Y, Lin J Q, Wilde S A, Sun D Y and Yang J H. Nature and signifieance of the Early Cretaceous giant igneouse vent in eastern China. Earth Planet. Sci. Lett.,2005,233:103-119
Wu F Y, Yang J H, Lo C H.The Jiamusi Massif:A Jurassic accretionaryterrane along the Western Pacific margin of NE China. Island Arc,2007,16:156-172
Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China. Journal of Asian Earth Sciences,2011,41:1-30
Xie X J. The surfacial geochemical expressions of Giant ore-deposits. In:Whiting, B H,Hodgson C J and Mason R (Editors), Giant Ore Deposits II, Queen's University, Kingston,1995,479-492
Xiong X L, Adam J, Green TH. Rutile stability and rutile/melt HFSE Partitioning during Partial melting ofhydrous basalt:im Plieations for. ITGgenesis. Chemieal Geology,2005,218:339-359
Zhang Z C, Mao J W, et al.,Geochemistry and geochronology of the volcanic rocks associated with the Dong'an adularia-sericite epithermal gold deposit, Lesser Hinggan Range, Heilingjiang province, NE China:Constrains on the metallogenesis. Ore Geology Reviews.2010,37:158-174
敖贵武,薛明轩,周辑,等.黑龙江东安金矿床成因探讨.矿产与地质.2004,18(2)：118-125
毕伏科,肖文暹,阎同生,等.成矿系列的缺位问题及其在成矿预测中的应用.矿床地质,2006,25(6)：735-742
边红业,陈满,刘洪利,等.黑龙江省逊克县高松山金矿床地质特征及成因分析.地质与资源,2009,18(2)：91-95
陈桂虎,王福州,王艳忠,等.黑龙江逊克—嘉荫地区金矿地质特征及找矿方向.黄金科学技术,2012,20(2)：14-23
陈国达.地洼学说.长沙：中南工业大学出版社,1996
陈国达.地洼学说—活化构造及成矿理论体系概论.北京：地质出版社,1997
陈静.黑龙江小兴安岭区域成矿背景与有色、贵金属矿床成矿作用：[博士学位论文].长春：吉林大学,2011
陈雷,孙景贵,陈行时,等.张广才岭东侧英城子金矿区早古生代花岗岩锆石U—Pb年龄及地质意义.地质学报,2009,83(9)：1327-1334
陈行时,张朋,孙景贵,等.张广才岭英城子金矿区早古生代花岗岩的元素地球化学特征、岩石成因及构造意义.吉林大学学报(地球科学版),2011,41(2)：441-447
陈衍景,张静,赖勇.大陆动力学与成矿作用.北京：地震出版社,2001
陈衍景,李诺.大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异.岩石学报,2009,25(10)：2477-2508
陈毓川,裴荣富,王登红.三论矿床的成矿系列问题.地质学报,2006,80(10)：1501-1507
陈文,张彦,金贵善,张岳桥.青藏高原东南缘晚新生代幕式抬升作用的Ar-Ar热年代学证据.岩石学报,2006,22(4)：867-872
揣媛媛,肖克炎,湛邵斌,等.基于SIG的证据权法矿产资源评价及应用.吉林大学学报(地球科学版),2007,37(1)：54-58
代军治,毛景文,杨富全,等.华北地台北缘燕辽铝(铜)成矿带矿床地质特征及动力学背景.矿床地质,2006,25(5)：598-612
邓晋福,刘厚祥,赵海玲等.燕辽地区燕山期火成岩与造山模型.现代地质,1996,10(2)：137-148
杜安道,赵敦敏,王淑贤,等.Carius管溶样—负离子热表面电离质谱准确测定辉钼矿铼—饿同位素地质年龄.岩矿测试,2001,20(4)：247-252
杜美艳,李超,杨乃峰,等.翠宏山铁多金属矿床成矿流体包裹体及硫同位素特征.世界地质,2011,30(4)：538-540
方维萱.秦岭造山带大型—超大型金属矿床形成大陆动力学条件分析.西北地质,1998,3l(3)：11-15
方维萱,张国伟,李亚林.南秦岭晚古生代伸展构造特征及意义.西北大学学报,2001,31(3)：235-240
范宏瑞,谢奕汉,翟明国,等.豫陕小秦岭脉状金矿床三期流体运移成矿作用.岩石学报,2003,20(1)：263-266
冯学仕,王尚彦,等.贵州省区域矿床成矿系列与成矿规律.北京：地质出版社,2004
高秉璋,洪大卫,郑基俭,等.花岗岩类区1：5万区域地质填图方法指南.北京：中国地质大学出版社,1991
高晓峰.东北地区中生代火成岩Sr-Nd-Pb同位素填图及其对区域构造演化的制约：[博士学位论文].北京：中国科学院研究生院,2007
高珍权,刘继顺,陈德兴.小秦岭西段架鹿金矿田成矿流体特征、物理化学条件及演化.地球化学,2001,30(3)：257-263
葛文春,李献华等.呼伦湖早白垩世碱性流纹岩的地球化学特征及其意义.地质科学,2001,36(2)：176-183
葛文春,吴福元,周长勇,等.大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及其地质意义.岩石学报,2005,21(3)：749-762
葛文春,吴福元,周长勇,等.兴蒙造山带东段斑岩型Cu、Mo矿床成矿时代及其地球动力学意义.科学通报,2007,52(2)：2407-2417
葛小月,李献华,周汉文.琼南晚白坐世基性岩墙群的年代学元素地球化学和Sr—Nd同位素研究.地球化学,2003,32(1)：11-20
郭继海,汪长生,石耀军.黑龙江东安金矿地质及地球化学特征.地质与勘探,2004,40(4)：37-44
郭嘉.黑龙江省霍吉河钼矿床地质特征及成因：[硕士学位论文].长春：吉林大学,2009
韩振哲,赵海玲,苏士杰,等小兴安岭东南金山屯—带晚三叠世二长花岗岩成因及其地质意义.现代地质,2008,22(2)：197-206
韩振哲,赵海玲,王盘喜,等.黑龙江省伊春地区晚三叠世—早侏罗世铝质A型正长—碱长花岗岩地球化学特征及其构造意义.岩石矿物学杂志,2009a,28(2)：97-108
韩振哲,赵海玲,李娟娟,等.黑龙江铁力兴安—带斑岩型钼矿资源潜力预测.地质与勘探,2009b,45(3)：253-259
韩振哲,金哲岩,吕军,等.小兴安岭东南鹿鸣—兴安—前进地区早中生代含矿花岗岩成岩成矿特征.地质与勘探,2010,45(3)：253-259
韩振哲.小兴安岭东南段早中生代花岗岩类时空演化特征与多金属成矿：[博士学位论文].北京：中国地质大学,2011
韩振新,郝正平,侯敏,等.黑龙江主要成矿带矿床成矿系列.哈尔滨：哈尔滨工程大学出版社,1996
韩振新,徐衍强,郑庆道,等.黑龙江省重要金属和非金属矿产的成矿系列及其演化.哈尔滨：黑龙江人民出版社,2004：150-160
何鹏,严光生,祝新友,等.青海赛什塘铜矿床流体包裹体研究.中国地质,2013,40(2)：580-593
何知礼.包裹体矿物学.北京：地质出版社,1982
黑龙江省地质矿产局.黑龙江省区域地质志.北京：地质出版社,1993
黑龙江省有色金属地质勘查703队.黑龙江省伊春市二股营林所、丰林林场幅1：5万区域地质矿产调查报告,2008
黑龙江省地质矿产局第三地质队.黑龙江省逊克县翠宏山铁多金属矿床普查—初勘地质报告.哈尔滨：黑龙江省地质矿产局地质矿产局地质三队,1984
胡瑞忠,毛景文,毕献武,等.浅谈大陆动力学与成矿关系研究的若干发展趋势.地球化学,2008,37(4)：344-352
黄典豪,杜安道,吴澄宇,等.华北地台钼(铜)矿床成矿年代学研究—辉铝矿铼—锇年龄及其地质意义.岩石学报,1996,15(4)：365-372
洪大卫,王式洸,韩宝福,等.碱性花岗岩的构造环境分类及其鉴别标志.中国科学(B辑),1995,25(4)：418-426
侯增谦.斑岩Cu-Mo-Au矿床：新认识与新进展.地学前缘,2004,3：131-144
侯增谦,曲晓明,杨竹森,等.青藏高原碰撞造山带：Ⅲ后碰撞伸展成矿作用.矿床地质,2006,19(3)：629-651
侯增谦.大陆碰撞成矿论.地质学报,2010,84(1)：30-52
华仁民.流体在金属矿床形成过程中的作用和意义—水-岩反应研究进展系列评述.南京大学学报(地球科学),1993,5(3)：351-360
华仁民.成矿过程中由流体混合而导致金属沉淀的研究.地球科学进展,1994,4(9)：15-22
黄朋,顾雪祥,唐菊兴.西藏玉龙斑岩铜(钼)矿金属迁移、沉淀机制探讨.四川地质学报,2000,19(2)：57-61
霍亮,孙丰月.黑龙江东安金矿床流体包裹体特征及矿床成因研究.黄金,2010,31(3)：8-14
贾维林,罗登春,嵇贵忠,等.黑龙江省铁力市鹿鸣钼多金属矿床普查报告.黑河：黑龙江省第五地质勘察院,2006
蒋少涌,杨竞红,赵葵东,等.金属矿床Re-Os同位素示踪与定年.南京大学学报(自然科学),2000,36(6)：669-677
李红阳,侯增谦.初论幔柱构造成矿体系.矿床地质,1998,17(3)：247-255
李林山,何财,李少云,等.黑龙江省伊春市霍吉河钼矿床地质特征及成因探讨.吉林地质,2010,29(2)：53-55
李诺,孙亚莉,李晶,等.内蒙古乌努格吐山斑岩铜钼矿床辉钼矿铼锇等时线年龄及其成矿动力学背景.岩石学报,2007,23(11)：2881-2886
李永飞.古亚洲洋构造体制与滨太平洋构造体制叠加转化研究项目报告.沈阳：沈阳地质调查中心,2013
刘宝山,马永强,吕军,等.伊春地区上游新村晚三叠世二长花岗岩体成因及就位机制.地质与资源,2005,14(3)：170-191
刘宝山,任凤和,李仰春,等.伊春地区晚印支期Ⅰ型花岗岩带特征及其构造背景.地质与勘探,2007,43(1)：74-78
刘斌.中高盐度NaCl-H2O包裹体的密度式和等容式及其应用.地质论评,2001,27(6)：617-621
刘桂阁,王恩德,常春郊,等.黑龙江省逊克县高松山金矿成因探讨.有色矿冶金,2006,22-24
刘红霞.黑龙江省伊春—延寿成矿带成矿系统分析与成矿预测：[硕十学位论文].长春：吉林大学,2007
刘伟.岩浆流体在热液矿床形成中的作用.地学前缘,2001,8(3)：204-215
刘智明,敖贵武,于建波,等.东安浅成低温热液型金矿床矿物学特征.地质找矿论丛,2004,19(3)：177-184
刘志宏.黑龙江省翠宏山钨钼锌多金属矿床地质特征及成因：[硕士学位论文].长春：吉林大学,2009
刘志逊,赵寒冬,马丽玲,等.小兴安岭晚石炭世花岗岩岩浆混合作用的岩相学证据及其地质意义.地质通报,2007,26(3)：289-298
梁福来.黑龙江省二股—翠宏山地区多金属矿床成矿条件和找矿方向：[硕士学位论文].长春：吉林大学,201l
卢焕章,李秉伦等.包裹体地球化学.北京：地质出版社,1990.162-215
卢焕章,范宏瑞,倪培,等.流体包裹体.北京：科学出版社,2004,1-486
罗照华,邓晋福,韩秀卿太行山造山带岩浆活动及其造山过程反演.北京：地质出版社,1999,124
罗照华,白志达,赵志丹等.塔里木盆地南北缘新生代火山岩成因及其地质意义.地学前缘,2003,10(3)：179-189
罗照华,梁涛,陈必河,等.板内造山作用与成矿.岩石学报,2007,23(8)：1945-1956
祁进平,陈衍景.东北地区浅成低温热液矿床的地质特征和构造背景.矿物岩石,2005,25(2)：47-59
屈文俊,杜安道.高温密闭溶样电感耦合等离子体质谱准确测定辉钼矿铼—饿地质年龄.岩矿测试,2003,22(4)：254-262
毛景文,张作衡,余金杰,等.华北及邻区中生代大规模成矿的地球动力学背景：从金属矿床年龄精测得到启示.中国科学(D辑),2003,33(4)：259-299
毛景文,谢桂青,张作衡,等.中国北方中生代大规模成矿作用的期次和相应的地球动力学环境.岩石学报,2005,21(1)：169-188
任纪舜.中国大地构造及其演化.北京：科学出版社,1980
芮宗瑶,侯增谦,李光明,等.俯冲—碰撞—深断裂和埃达克岩与斑岩铜矿.地质与勘探,2006,42(1)：1-6
邵沽连.金矿找矿矿物学.武汉：中国地质大学出版社,1988
邵军,赵山,马启波.黑龙江小兴安岭—张广才岭成矿带铅锌多金属成矿规律研究.沈阳：沈阳地质调查中心,2006
邵军,李秀荣,杨宏智.黑龙江翠宏山铅锌多金属矿区花岗岩锆石SHRIMP U-Pb测年及其地质意义.岩石学报,2011,32(2)：163-170
沈阳地质矿产研究所.小兴安岭—张广才岭花岗岩带的形成与演化.沈阳：沈阳地质调查中心,1991
时永明,崔彬,贾维林.黑龙江省铁力市鹿鸣钼矿床地质特征.地质与勘探,2007,43(2)：19-22
舒广龙.湖北丰山矿田成矿地质背景及斑岩成矿系列与微细浸染型金矿：[博士学位论文].湖南：中南大学,2004
舒广龙,马诗敏,刘继顺.基于斑岩成矿体系结构的深部找矿预测.地质与勘探.2007,43(2)：1-7
孙德有.张广才岭中生代花岗岩成因及其地球动力学意义：[博士学位论文].长春：吉林大学,2001
孙德有,吴福元,高山,等.小兴安岭东部清水岩体的锆石激光探针U—Pb年龄测定.地球学报,2004,25(2)：213-218
孙丰月.胶东地区中新生代区域构造演化与成矿.长春地质学院学报,1994.24(4)：378-384
孙丰月,金巍,李碧乐,等.关于热液脉状金矿成矿深度的思考.长春科技大学学报地球科学版,2000,30(增刊)：27-30
陶卫星,齐永生,刘学波.逊克县东安金矿矿床成因及找矿标志.吉林地质,2006,25(3)：29-34
谭成印.黑龙江省主要金属矿产构造—成矿系统基本特征：[博士学位论文].北京：中国地质大学,2009
谭红艳,舒广龙,吕骏超,等小兴安岭鹿鸣大型钼矿LA-ICP-MS锆石U—Pb和辉钼矿Re-Os年龄及其地质意义.吉林大学学报(地球科学版),2012,42(6)：1757-1770
谭红艳,汪道东,吕骏超,等.小兴安岭霍吉河钼矿床成岩成矿年代学及其地质意义.岩石矿物学杂志,2013,32(5)：730-750
唐文龙.黑龙江省前进地区岩浆岩地球化学特征与成矿预测：[硕士学位论文].长春：吉林大学,2007
唐忠,叶松青,杨言辰.黑龙江逊克高松山金矿成因模式.世界地质,2010,29(3)：400-407
王登红,地慢柱及其成矿作用.北京：地震出版社,1998
王世称,王於天.综合信息解译原理与矿产预测图编制方法.长春：吉林大学出版社,1989
王世称,叶水盛,等.综合信息成矿系列预测专家系统.长春：长春出版社,1999
王世称,陈永良,夏立显.综合信息矿产预测理论与方法.北京：科学出版社,2000
王艳忠,郎利国,于明军.高松山金矿区地质、物化探特征及找矿方向.吉林地质,2006,25(2)：36-40
王义天,毛景文.碰撞造山作用期后伸展体制下的成矿作用—以小秦岭金矿集中区为例.地质通报,2002,21(8-9)：562-566
魏玉明,何财,刘文,等.黑龙江省逊克县霍吉河钼矿床勘探报告.佳木斯：黑龙江省第六地质勘察院,2009
吴福元,孙德有,林强.东北地区显生宙花岗岩的成因与地壳增生.岩石学报,1999,5(2)：181-189
吴小军.黑龙江省前进东山铅锌矿床地质特征及成因：[硕士学位论文].长春：吉林大学,2008
武子玉,王洪波等,黑龙江黑河三道湾子金矿床地质地球化学研究.地质论评,2005,51(3)：264-267
阎鸿铨,杨铭埙等.黑龙江省伊春佳木斯地块西缘地质及块状硫化物铅锌矿床.哈尔滨：黑龙江科学技术出版社,1994
肖克炎,丁建华,刘锐.美国“三步式”固体矿产资源潜力评价方法评述.地质论评,2006,52(6)：793-798.
谢学锦,王学求.金的勘查地球化学.济南：山东科学技术出版社,2000
薛明轩,刘明,双宝.黑龙江大安河金矿控矿条件及成矿机理分析.世界地质,2001,20(1)：34-39
薛明轩,叶松青,刘智明,等.黑龙江东安金矿床地质地球化学特征初探.黄金,2002,23(7)：1-7
徐克勤,胡受奚,孙明志,等.华南两个成因系列花岗岩及其成矿特征.矿床地质,1982,(2)：1-14
徐杰,高战武,孙建宝,等.区域伸展体制下盆山构造耦合关系的探讨.地质学报,2001,75(2)：165-173
姚书振,丁振举,周宗桂.初论造山带成矿学.地质科技情报,2002,21(4)：1-6
阎鸿铨,杨锡埙,张贻侠,等.黑龙江省伊春佳木斯地块西缘地质及块状硫化物铅锌矿床.哈尔滨：黑龙江科学技术出版社,1994
杨铁铮.小兴安岭地区尔安金矿区火山岩及其与金矿关系研究：[硕十学位论文].北京：中国地质大学,2008
杨言辰.黑龙江小兴安岭—张广才岭成矿带金、多金属矿床成矿规律与成矿预测：[博士学位论文].长春：吉林大学,2005
叶会寿,毛景文,李永峰,等.东秦岭东沟超大型斑岩钼矿SHRIMP锆石U—Pb和辉钼矿Re—Os年龄及其地质意义.地质学报,2006,780(7)：1078-1086
叶天竺,肖克炎,严光生.矿床模型综合地质信息预测技术研究.地学前缘,2007,14(5)：11-19
叶鑫.黑龙江省逊克县东安金矿矿床地质特征及成因研究：[硕士学位论文].长春：吉林大学,2011
尹冰川,冉清昌.小兴安岭—张广才岭地区区域成矿演化.矿床地质,1997,16(3)：235-242
于建波,苏仁奎,刘智明.东安金矿床控矿因素及成矿物质来源浅析.黄金科学技术,2005,13(6)：8-11
翟裕生,姚书振,林新多,等.长江中下游地区铁铜(金)成矿规律.北京：地质出版社,1992,1-234
翟裕生,姚书振,崔斌,等.成矿系列研究.武汉：中国地质大学出版社,1996：1-192
翟裕生,邓军,李晓波.区域成矿学.北京：地质出版社,1999
翟裕生.论成矿系统.地学前缘,1999,6(1)：13-28
翟裕生,吕古贤.构造动力体制转换与成矿作用.地球学报,2002,23(2)：97-102
翟裕生.成矿系统研究与找矿.地质调查与研究,2003,26(2)：65-72
翟裕生.地球系统科学与成矿学研究.地学前缘,2004,11(1)：1-10
张德会.流体的沸腾和混合在热液成矿中的意义.地球科学进展,1997,12(6)：546-552.
张海驲.黑龙江省印支期花岗岩的确定及其构造意义.黑龙江地质,1991,2(1)：8-18
张炯飞,李之彤,金成沫.中国东北部地区埃达克岩及其成矿意义.岩石学报,2004,20(2)：361-368
张理刚.稳定同位素在地质科学中的应用.西安：陕西科学技术出版社,1985,1-10
张旗,王焰,刘伟,等.埃达克岩的特征及其意义.地质通报,2002,21(7)：431-435
张旗,王焰,刘红涛,等.中国埃达克岩的时空分布及其形成背景.地学前缘,2003,10(4)：385-400
张旗,王焰,李承东等.花岗岩的Sr-Yb分类及其地质意义.岩石学报,2006,22：2249-2260
张旗,金惟俊,李承东,等.中国东部燕山期大规模岩浆活动与岩石圈减薄与大火成岩省的关系.地学前缘,2009,16(2)：21-51
张旗,李承东,等.花岗岩：地球动力学意义.北京：海洋出版社,2012,1-275
张苏江.黑龙江省铁力地区铝(铜)矿床成矿地质条件及找矿潜力分析：[硕士学位论文].长春：吉林大学,2009
张兴洲,杨宝俊,吴福元,等.中国兴蒙—吉黑地区岩石圈结构基本特征.中国地质,2006,33(4)：816-823.
张彦,陈文,陈克龙,刘新宇.成岩混层(I/S) Ar-Ar年龄谱型及39Ar核反冲丢失机理研究—以浙江长兴地区P-T界线粘土岩为例.地质论评,2006,52(4)：556-561
张昱.黑龙江省东部早中生代火成岩构造组合及其大地构造演化：[博士学位论文].北京：中国地质大学(北京),2008
张振庭.黑龙江省伊春地区铅锌多金属矿产预测：[硕士学位论文].长春：吉林大学,2010
张遵忠,吴昌志,顾连星,等.燕辽成矿带东段新台门钼矿床Re-Os同位素年龄及其地质意义.矿床地质,2009,28(3)：313-320
赵春荆,彭玉鲸,党增欣,等.吉黑东部构造格架及地壳演化.沈阳：辽宁大学出版社,1996
赵洪海,薛继广,连永牢.黑龙江省逊克县高松山矿区1号矿脉岩金详查报告.牡丹江：武警黄金第一总队,2011
赵鹏大,陈永清,刘吉平,等.地质异常成矿预测理论与实践.武汉：中国地质大学出版社,1999
赵一鸣,毕承思,邹晓秋,等.黑龙江多宝山铜山大型斑岩铜(铝)矿床中辉铝矿的铼—锇同位素年龄.地球化学,1997,18(1)：61-67
赵志丹,莫宣学,张双全等.西藏中部乌郁盆地碰撞后岩浆作用—特提斯洋壳俯冲再循环的证据.中国科学(D辑),2001,31(增刊)：20-26
周佐民.碱质A型花岗岩的判别、成因与构造环境.华南地质与矿产,2011,27(3)：216-220
Alok Porwal,Emmanuel John M Carranza,Martin Hale. A hybridfuzzy wights-of-evidence model for mineral potential mapping. Natural Resources Research,2006,15(1):1-14
Badham J P N. Strike-sliporogens-an expantion for the Hereynides. Geol. Soc. London,1982,139:493-504
Barley M E.,Groves D I. Supercontinent cycles and the distribution of metal deposits through time. Geology,1992,20:291-294
Barnes H L. Energetics of Hydrothermal Ore Deposits in Frontiers in Geochemistry:Organic, Solution and Ore Deposit Geochemistry. Columbia:Bellwether Publishing,Ltd,2002,184-190
Bilibin Y A. Metallogenic Provinces and Metallogenic Epochs. New York:Queenscoll Flushing,1955,35
Bonham,Carter G F. Geographic Information Systems for Geoscientist:Modelling with GIS. Oxford:Linacre House,1994:317-337
Chen J P, Wang G W, Hou C B.Quantitative Prediction and Evaluation of Mineral Resources Based on GIS:A Case Study in Sanjiang Region,Southwestern China. Natural Resources Research,2005,14(4):285-294
Chen Y J.Mineralization during collisional orogenesis and its control of the distribution of gold deposits in Junggar Mountains, Xinjiang, China. Acta Geologica Sinica,1997,71(1):69-79
Christensen J N, Halliday A N, Leigh K E, et al. Direct dating of sulfides by Rb-Sr:Acritical test using the Polaris Mississippi Valley-type Zn-Pb deposit. Geochimica. et Cosmochimica. Acta,1995,59:5191-5197
Condie K C. Mantle plume and their record in earth history. London:Cambridge University Press,2001
Corbett G J, Leach T M. Southwest Pacific Rim gold-copper systems:structure, alteration and mineralization. Society of Economic Geologists Special Publication,1998,6:1-240
Cline J S. Bodnar R J. Can economic porphyry copper mineralization be generated by a typical calc-alkaline melt. Geophys Res,1991,96:8113-8126
De Grave J, Buslov M M and Van den haute P. Distante ects of India-Eurasia convergence and Mesozoic intracontinental deformation in Central Asia:Constraints from apatite? ssion-track thermochronoloy.Journal of Asian Earth Seiences,2007,29:188-204
Fang W X, Zhang G W, Lu J Y, et al. Complexity and geodynamics of ore-accumulating basin in the Qinling orogenic belt, China. Act a Geo Sinica,2000,74(3):458-465
Gill J B. Orogenie Andesites and Piate Tectonies. Berlin:Springer-Verlag,1981,358-360
Goldfarb R J, Philips G N, Nokleberg W J. Tectonic setting of synorogenic gold deposits of the Pacific Rim. Ore Geology Reviews,1998,13:185-218
Goldfarb R J, Geoves D I,Gardoll S. Orogenic gold and geologictime:A global synthesis. Ore Geology Reviews,2001,18:1-75
Groves D I, Goldfarb R J, Gebre-Maiam M,et al. Orogenic gold deposits:A proposed classification in the context of their crustal distribution and relationship to other gold deposit types. Ore Geology Reviews, 1998,13:7-27
Groves D I, Goldfarb R J, Knox-Robinson C M, et al. Late kinematic timing of orogenic gold deposits and significance for computer-based exploration techniques with emphasison the Yilgarn Block, Weatern Australia. Ore Geology Reviews,2000,17:1-38
Grove D I, Condie K C, Goldfarb R J, Hronsky J M A, Vielreicher R M. Secular changes in golobal tectonic processes and their influence on the temporal distribution of gold-bearing mineral deposits. Economic Geology 100th Anniversary Volume,2005,203-224
Groves D I, Bierlein F P. Geodynamic settings of mineral deposit systems. Journal of the Geological Society, London,2007,164:19-30
Hall, D.L., S.M. Sterner and R.J. Bodnar. Freezing point depression of NaCl-KCl-H2O solutions. Econ.Geol. 1988,83:197-202
Hartmann L A, Delgado I M. Cratons and orogenic belts of the Brazilian shield and their contained gold deposits. Mineralium Deposita,2001,36(34):207-217
Hedenquist J W, Lowenstern J B. The role of magmas in the formation of hydrothermal ore deposits. Nature,1994,370(4):519-527
Henley R W, Ellis A J.Geothermal systems ancient and modern:a geochemical review.Earth Sci Rev, 1983,19:1-50
Huang D H, Du A D, Wu C Y, et al. Metallochronology of molybdenum (-copper) deposits in the north China platform:Re-Os age of molybdenite and its geological significance. Mineral Deposits,1996,15 (4):365-372
Hu Z C, Liu Y S, Gao S, et al. A local aerosol extraction strategy for the determination of the aerosol composition in LA-ICP-MS. Journal of Analytical Atomic Spectrometry,2008,23:1192-1203
Hugh R.R. Using geochemical data:Evaluation, Presentation, UK:Interpretation. Pearson Education Limited.1993
Kerrich R, Goldfarb R,Groves D, Garwin S. The characteristics, origins,and geodynamic settings of supergiant gold metallogenic provinces. Science in China,2001,43:1-68
Kerrich R, Goldfarb R J, Richards J. Metallogenic provinces in an evolving geodynamic framework. Economic Geology 100th Anniversary Volume,2005,1097-1136
Leach D L, Sangster D F, Kelley K D, Large R R, Garven G, Allen C R, Gatzmer J.Wallters S. Sediment-Hosted Lead-Zink Deposit:A Global Perspective. Economic Geology 100th Anniversary Volume,2005, 561-607
Ludwig, K R. ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel. Berkeley:Berkeley Geochronology Center, California,2003
Mao J W, Zhang Z H. Re-Os Isotopic dating of molybdenites in the Xiaoliugou W(Mo) deposit in the Northern Qilian Mountains and its geological significance. Geochimica et Cosmochimica Acta,1999,63(11/12):1815-1818
Mitchell A H G, Garson M S. Mineral Deposits and Global Tectonic Settings. London:Academic Press,1981, 1-405
Nakai S, Halliday A N,Kesler S E, et al. Rb-Sr dating of sphalerite and genesis of MVT deposits. Nature, 1990,346:354-357
Nakai S, Halliday A N, Kesler S E, et al. Rb-Sr dating of sphalerites from Mississippi Valley-type(MVT) ore deposits. Geochimica. et Cosmochimica. Acta,1993,57:417-427
Sawkins J. Metal Deposits in Relation to Plate Tectonic. Berlin:Springer-Verlag,1984,283-294
Sheppard S M F, Nielsen R L, Taylor H P. Hydrogen and oxygen isotope ratios in minerals from porphyry copper deposits. Econ Geol,1971,66:515-542
Sillitoe RH, Perello J. Andean copper province:tectonomagmatic settings. Economic Geology 100th Annivers ary volume,2005,845-890
Sillitoe RH, Mortensen JK. Longevity of porphyry copper formation at Quellaveco, Peru. Economic Geology, 2010a,105:1157-1162
Sillitoe RH. Porphyry copper systems. Economic Geology,2010b,105:2-41
Singer D A. Basic concepts in three-part quantitative assessments of undiscovered mineral resources. Nonrenewable Resources,1993,2(2):69-81
Sobel E R,Chen J and Heermance R V. Late Oligocene-Early Miocene initiation of shortening in the Southwestern Chinese Tian Shan:Implications for Neogene shortening rate variations.Earth and Planetary Seience Letters,2006,247:70-81
Stein H J, Markey R J, Morgan J W, Du A, Sun Y. Highly precise and accurate Re-Os ages for molybdenum from the East Qinling molybdenum belt, Shanxi Province, China. Economic Geology.1997,98:175-180
Steiger, R.H. and Jager, E. Subcommission on geochronology:convention on the use of decay constants in geo-and cosmochronology. Earth Planet. Sci. Lett.,1977,36:359-362
Sterner S M, et al. Synthetic fluid inclusions:V. Solubility relations in the system NaCl-KCl-H2O under vapor-aaturated eonditions. Geochim.Cosmochim. Acta,1988,52:989-1005.
Titley S R, Beane R E. Porphyry copper deposits Part I.Geologic settings, petrology and tectogenesis. Econ Geol,1981,75:214-269
Wu F Y, Jahn B M, Wilde S A and D Y. Phanerozoic crustal growth:U-Pb and Sr-Nd isotoie evidence From the granites in northeastern China.TeetonoPhysies,2000,328:89-113
Wu F Y. Sun D Y, Li H M, et al. A-type ganites in northeastern China:age and geoehemical constraints on their petrogenesis. Chemical Geology,2002,187:143-173
Wu F Y, Lin J Q, Wilde S A, Sun D Y and Yang J H. Nature and signifieance of the Early Cretaceous giant igneouse vent in eastern China. Earth Planet. Sci. Lett.,2005,233:103-119
Wu F Y, Yang J H, Lo C H.The Jiamusi Massif:A Jurassic accretionaryterrane along the Western Pacific margin of NE China. Island Arc,2007,16:156-172
Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China. Journal of Asian Earth Sciences,2011,41:1-30
Xie X J. The surfacial geochemical expressions of Giant ore-deposits. In:Whiting, B H,Hodgson C J and Mason R (Editors), Giant Ore Deposits II, Queen's University, Kingston,1995,479-492
Xiong X L, Adam J, Green TH. Rutile stability and rutile/melt HFSE Partitioning during Partial melting ofhydrous basalt:im Plieations for. ITGgenesis. Chemieal Geology,2005,218:339-359
Zhang Z C, Mao J W, et al.,Geochemistry and geochronology of the volcanic rocks associated with the Dong'an adularia-sericite epithermal gold deposit, Lesser Hinggan Range, Heilingjiang province, NE China:Constrains on the metallogenesis. Ore Geology Reviews.2010,37:158-174
敖贵武,薛明轩,周辑,等.黑龙江东安金矿床成因探讨.矿产与地质.2004,18(2)：118-125
毕伏科,肖文暹,阎同生,等.成矿系列的缺位问题及其在成矿预测中的应用.矿床地质,2006,25(6)：735-742
边红业,陈满,刘洪利,等.黑龙江省逊克县高松山金矿床地质特征及成因分析.地质与资源,2009,18(2)：91-95
陈桂虎,王福州,王艳忠,等.黑龙江逊克—嘉荫地区金矿地质特征及找矿方向.黄金科学技术,2012,20(2)：14-23
陈国达.地洼学说.长沙：中南工业大学出版社,1996
陈国达.地洼学说—活化构造及成矿理论体系概论.北京：地质出版社,1997
陈静.黑龙江小兴安岭区域成矿背景与有色、贵金属矿床成矿作用：[博士学位论文].长春：吉林大学,2011
陈雷,孙景贵,陈行时,等.张广才岭东侧英城子金矿区早古生代花岗岩锆石U—Pb年龄及地质意义.地质学报,2009,83(9)：1327-1334
陈行时,张朋,孙景贵,等.张广才岭英城子金矿区早古生代花岗岩的元素地球化学特征、岩石成因及构造意义.吉林大学学报(地球科学版),2011,41(2)：441-447
陈衍景,张静,赖勇.大陆动力学与成矿作用.北京：地震出版社,2001
陈衍景,李诺.大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异.岩石学报,2009,25(10)：2477-2508
陈毓川,裴荣富,王登红.三论矿床的成矿系列问题.地质学报,2006,80(10)：1501-1507
陈文,张彦,金贵善,张岳桥.青藏高原东南缘晚新生代幕式抬升作用的Ar-Ar热年代学证据.岩石学报,2006,22(4)：867-872
揣媛媛,肖克炎,湛邵斌,等.基于SIG的证据权法矿产资源评价及应用.吉林大学学报(地球科学版),2007,37(1)：54-58
代军治,毛景文,杨富全,等.华北地台北缘燕辽铝(铜)成矿带矿床地质特征及动力学背景.矿床地质,2006,25(5)：598-612
邓晋福,刘厚祥,赵海玲等.燕辽地区燕山期火成岩与造山模型.现代地质,1996,10(2)：137-148
杜安道,赵敦敏,王淑贤,等.Carius管溶样—负离子热表面电离质谱准确测定辉钼矿铼—饿同位素地质年龄.岩矿测试,2001,20(4)：247-252
杜美艳,李超,杨乃峰,等.翠宏山铁多金属矿床成矿流体包裹体及硫同位素特征.世界地质,2011,30(4)：538-540
方维萱.秦岭造山带大型—超大型金属矿床形成大陆动力学条件分析.西北地质,1998,3l(3)：11-15
方维萱,张国伟,李亚林.南秦岭晚古生代伸展构造特征及意义.西北大学学报,2001,31(3)：235-240
范宏瑞,谢奕汉,翟明国,等.豫陕小秦岭脉状金矿床三期流体运移成矿作用.岩石学报,2003,20(1)：263-266
冯学仕,王尚彦,等.贵州省区域矿床成矿系列与成矿规律.北京：地质出版社,2004
高秉璋,洪大卫,郑基俭,等.花岗岩类区1：5万区域地质填图方法指南.北京：中国地质大学出版社,1991
高晓峰.东北地区中生代火成岩Sr-Nd-Pb同位素填图及其对区域构造演化的制约：[博士学位论文].北京：中国科学院研究生院,2007
高珍权,刘继顺,陈德兴.小秦岭西段架鹿金矿田成矿流体特征、物理化学条件及演化.地球化学,2001,30(3)：257-263
葛文春,李献华等.呼伦湖早白垩世碱性流纹岩的地球化学特征及其意义.地质科学,2001,36(2)：176-183
葛文春,吴福元,周长勇,等.大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及其地质意义.岩石学报,2005,21(3)：749-762
葛文春,吴福元,周长勇,等.兴蒙造山带东段斑岩型Cu、Mo矿床成矿时代及其地球动力学意义.科学通报,2007,52(2)：2407-2417
葛小月,李献华,周汉文.琼南晚白坐世基性岩墙群的年代学元素地球化学和Sr—Nd同位素研究.地球化学,2003,32(1)：11-20
郭继海,汪长生,石耀军.黑龙江东安金矿地质及地球化学特征.地质与勘探,2004,40(4)：37-44
郭嘉.黑龙江省霍吉河钼矿床地质特征及成因：[硕士学位论文].长春：吉林大学,2009
韩振哲,赵海玲,苏士杰,等小兴安岭东南金山屯—带晚三叠世二长花岗岩成因及其地质意义.现代地质,2008,22(2)：197-206
韩振哲,赵海玲,王盘喜,等.黑龙江省伊春地区晚三叠世—早侏罗世铝质A型正长—碱长花岗岩地球化学特征及其构造意义.岩石矿物学杂志,2009a,28(2)：97-108
韩振哲,赵海玲,李娟娟,等.黑龙江铁力兴安—带斑岩型钼矿资源潜力预测.地质与勘探,2009b,45(3)：253-259
韩振哲,金哲岩,吕军,等.小兴安岭东南鹿鸣—兴安—前进地区早中生代含矿花岗岩成岩成矿特征.地质与勘探,2010,45(3)：253-259
韩振哲.小兴安岭东南段早中生代花岗岩类时空演化特征与多金属成矿：[博士学位论文].北京：中国地质大学,2011
韩振新,郝正平,侯敏,等.黑龙江主要成矿带矿床成矿系列.哈尔滨：哈尔滨工程大学出版社,1996
韩振新,徐衍强,郑庆道,等.黑龙江省重要金属和非金属矿产的成矿系列及其演化.哈尔滨：黑龙江人民出版社,2004：150-160
何鹏,严光生,祝新友,等.青海赛什塘铜矿床流体包裹体研究.中国地质,2013,40(2)：580-593
何知礼.包裹体矿物学.北京：地质出版社,1982
黑龙江省地质矿产局.黑龙江省区域地质志.北京：地质出版社,1993
黑龙江省有色金属地质勘查703队.黑龙江省伊春市二股营林所、丰林林场幅1：5万区域地质矿产调查报告,2008
黑龙江省地质矿产局第三地质队.黑龙江省逊克县翠宏山铁多金属矿床普查—初勘地质报告.哈尔滨：黑龙江省地质矿产局地质矿产局地质三队,1984
胡瑞忠,毛景文,毕献武,等.浅谈大陆动力学与成矿关系研究的若干发展趋势.地球化学,2008,37(4)：344-352
黄典豪,杜安道,吴澄宇,等.华北地台钼(铜)矿床成矿年代学研究—辉铝矿铼—锇年龄及其地质意义.岩石学报,1996,15(4)：365-372
洪大卫,王式洸,韩宝福,等.碱性花岗岩的构造环境分类及其鉴别标志.中国科学(B辑),1995,25(4)：418-426
侯增谦.斑岩Cu-Mo-Au矿床：新认识与新进展.地学前缘,2004,3：131-144
侯增谦,曲晓明,杨竹森,等.青藏高原碰撞造山带：Ⅲ后碰撞伸展成矿作用.矿床地质,2006,19(3)：629-651
侯增谦.大陆碰撞成矿论.地质学报,2010,84(1)：30-52
华仁民.流体在金属矿床形成过程中的作用和意义—水-岩反应研究进展系列评述.南京大学学报(地球科学),1993,5(3)：351-360
华仁民.成矿过程中由流体混合而导致金属沉淀的研究.地球科学进展,1994,4(9)：15-22
黄朋,顾雪祥,唐菊兴.西藏玉龙斑岩铜(钼)矿金属迁移、沉淀机制探讨.四川地质学报,2000,19(2)：57-61
霍亮,孙丰月.黑龙江东安金矿床流体包裹体特征及矿床成因研究.黄金,2010,31(3)：8-14
贾维林,罗登春,嵇贵忠,等.黑龙江省铁力市鹿鸣钼多金属矿床普查报告.黑河：黑龙江省第五地质勘察院,2006
蒋少涌,杨竞红,赵葵东,等.金属矿床Re-Os同位素示踪与定年.南京大学学报(自然科学),2000,36(6)：669-677
李红阳,侯增谦.初论幔柱构造成矿体系.矿床地质,1998,17(3)：247-255
李林山,何财,李少云,等.黑龙江省伊春市霍吉河钼矿床地质特征及成因探讨.吉林地质,2010,29(2)：53-55
李诺,孙亚莉,李晶,等.内蒙古乌努格吐山斑岩铜钼矿床辉钼矿铼锇等时线年龄及其成矿动力学背景.岩石学报,2007,23(11)：2881-2886
李永飞.古亚洲洋构造体制与滨太平洋构造体制叠加转化研究项目报告.沈阳：沈阳地质调查中心,2013
刘宝山,马永强,吕军,等.伊春地区上游新村晚三叠世二长花岗岩体成因及就位机制.地质与资源,2005,14(3)：170-191
刘宝山,任凤和,李仰春,等.伊春地区晚印支期Ⅰ型花岗岩带特征及其构造背景.地质与勘探,2007,43(1)：74-78
刘斌.中高盐度NaCl-H2O包裹体的密度式和等容式及其应用.地质论评,2001,27(6)：617-621
刘桂阁,王恩德,常春郊,等.黑龙江省逊克县高松山金矿成因探讨.有色矿冶金,2006,22-24
刘红霞.黑龙江省伊春—延寿成矿带成矿系统分析与成矿预测：[硕十学位论文].长春：吉林大学,2007
刘伟.岩浆流体在热液矿床形成中的作用.地学前缘,2001,8(3)：204-215
刘智明,敖贵武,于建波,等.东安浅成低温热液型金矿床矿物学特征.地质找矿论丛,2004,19(3)：177-184
刘志宏.黑龙江省翠宏山钨钼锌多金属矿床地质特征及成因：[硕士学位论文].长春：吉林大学,2009
刘志逊,赵寒冬,马丽玲,等.小兴安岭晚石炭世花岗岩岩浆混合作用的岩相学证据及其地质意义.地质通报,2007,26(3)：289-298
梁福来.黑龙江省二股—翠宏山地区多金属矿床成矿条件和找矿方向：[硕士学位论文].长春：吉林大学,201l
卢焕章,李秉伦等.包裹体地球化学.北京：地质出版社,1990.162-215
卢焕章,范宏瑞,倪培,等.流体包裹体.北京：科学出版社,2004,1-486
罗照华,邓晋福,韩秀卿太行山造山带岩浆活动及其造山过程反演.北京：地质出版社,1999,124
罗照华,白志达,赵志丹等.塔里木盆地南北缘新生代火山岩成因及其地质意义.地学前缘,2003,10(3)：179-189
罗照华,梁涛,陈必河,等.板内造山作用与成矿.岩石学报,2007,23(8)：1945-1956
祁进平,陈衍景.东北地区浅成低温热液矿床的地质特征和构造背景.矿物岩石,2005,25(2)：47-59
屈文俊,杜安道.高温密闭溶样电感耦合等离子体质谱准确测定辉钼矿铼—饿地质年龄.岩矿测试,2003,22(4)：254-262
毛景文,张作衡,余金杰,等.华北及邻区中生代大规模成矿的地球动力学背景：从金属矿床年龄精测得到启示.中国科学(D辑),2003,33(4)：259-299
毛景文,谢桂青,张作衡,等.中国北方中生代大规模成矿作用的期次和相应的地球动力学环境.岩石学报,2005,21(1)：169-188
任纪舜.中国大地构造及其演化.北京：科学出版社,1980
芮宗瑶,侯增谦,李光明,等.俯冲—碰撞—深断裂和埃达克岩与斑岩铜矿.地质与勘探,2006,42(1)：1-6
邵沽连.金矿找矿矿物学.武汉：中国地质大学出版社,1988
邵军,赵山,马启波.黑龙江小兴安岭—张广才岭成矿带铅锌多金属成矿规律研究.沈阳：沈阳地质调查中心,2006
邵军,李秀荣,杨宏智.黑龙江翠宏山铅锌多金属矿区花岗岩锆石SHRIMP U-Pb测年及其地质意义.岩石学报,2011,32(2)：163-170
沈阳地质矿产研究所.小兴安岭—张广才岭花岗岩带的形成与演化.沈阳：沈阳地质调查中心,1991
时永明,崔彬,贾维林.黑龙江省铁力市鹿鸣钼矿床地质特征.地质与勘探,2007,43(2)：19-22
舒广龙.湖北丰山矿田成矿地质背景及斑岩成矿系列与微细浸染型金矿：[博士学位论文].湖南：中南大学,2004
舒广龙,马诗敏,刘继顺.基于斑岩成矿体系结构的深部找矿预测.地质与勘探.2007,43(2)：1-7
孙德有.张广才岭中生代花岗岩成因及其地球动力学意义：[博士学位论文].长春：吉林大学,2001
孙德有,吴福元,高山,等.小兴安岭东部清水岩体的锆石激光探针U—Pb年龄测定.地球学报,2004,25(2)：213-218
孙丰月.胶东地区中新生代区域构造演化与成矿.长春地质学院学报,1994.24(4)：378-384
孙丰月,金巍,李碧乐,等.关于热液脉状金矿成矿深度的思考.长春科技大学学报地球科学版,2000,30(增刊)：27-30
陶卫星,齐永生,刘学波.逊克县东安金矿矿床成因及找矿标志.吉林地质,2006,25(3)：29-34
谭成印.黑龙江省主要金属矿产构造—成矿系统基本特征：[博士学位论文].北京：中国地质大学,2009
谭红艳,舒广龙,吕骏超,等小兴安岭鹿鸣大型钼矿LA-ICP-MS锆石U—Pb和辉钼矿Re-Os年龄及其地质意义.吉林大学学报(地球科学版),2012,42(6)：1757-1770
谭红艳,汪道东,吕骏超,等.小兴安岭霍吉河钼矿床成岩成矿年代学及其地质意义.岩石矿物学杂志,2013,32(5)：730-750
唐文龙.黑龙江省前进地区岩浆岩地球化学特征与成矿预测：[硕士学位论文].长春：吉林大学,2007
唐忠,叶松青,杨言辰.黑龙江逊克高松山金矿成因模式.世界地质,2010,29(3)：400-407
王登红,地慢柱及其成矿作用.北京：地震出版社,1998
王世称,王於天.综合信息解译原理与矿产预测图编制方法.长春：吉林大学出版社,1989
王世称,叶水盛,等.综合信息成矿系列预测专家系统.长春：长春出版社,1999
王世称,陈永良,夏立显.综合信息矿产预测理论与方法.北京：科学出版社,2000
王艳忠,郎利国,于明军.高松山金矿区地质、物化探特征及找矿方向.吉林地质,2006,25(2)：36-40
王义天,毛景文.碰撞造山作用期后伸展体制下的成矿作用—以小秦岭金矿集中区为例.地质通报,2002,21(8-9)：562-566
魏玉明,何财,刘文,等.黑龙江省逊克县霍吉河钼矿床勘探报告.佳木斯：黑龙江省第六地质勘察院,2009
吴福元,孙德有,林强.东北地区显生宙花岗岩的成因与地壳增生.岩石学报,1999,5(2)：181-189
吴小军.黑龙江省前进东山铅锌矿床地质特征及成因：[硕士学位论文].长春：吉林大学,2008
武子玉,王洪波等,黑龙江黑河三道湾子金矿床地质地球化学研究.地质论评,2005,51(3)：264-267
阎鸿铨,杨铭埙等.黑龙江省伊春佳木斯地块西缘地质及块状硫化物铅锌矿床.哈尔滨：黑龙江科学技术出版社,1994
肖克炎,丁建华,刘锐.美国“三步式”固体矿产资源潜力评价方法评述.地质论评,2006,52(6)：793-798.
谢学锦,王学求.金的勘查地球化学.济南：山东科学技术出版社,2000
薛明轩,刘明,双宝.黑龙江大安河金矿控矿条件及成矿机理分析.世界地质,2001,20(1)：34-39
薛明轩,叶松青,刘智明,等.黑龙江东安金矿床地质地球化学特征初探.黄金,2002,23(7)：1-7
徐克勤,胡受奚,孙明志,等.华南两个成因系列花岗岩及其成矿特征.矿床地质,1982,(2)：1-14
徐杰,高战武,孙建宝,等.区域伸展体制下盆山构造耦合关系的探讨.地质学报,2001,75(2)：165-173
姚书振,丁振举,周宗桂.初论造山带成矿学.地质科技情报,2002,21(4)：1-6
阎鸿铨,杨锡埙,张贻侠,等.黑龙江省伊春佳木斯地块西缘地质及块状硫化物铅锌矿床.哈尔滨：黑龙江科学技术出版社,1994
杨铁铮.小兴安岭地区尔安金矿区火山岩及其与金矿关系研究：[硕十学位论文].北京：中国地质大学,2008
杨言辰.黑龙江小兴安岭—张广才岭成矿带金、多金属矿床成矿规律与成矿预测：[博士学位论文].长春：吉林大学,2005
叶会寿,毛景文,李永峰,等.东秦岭东沟超大型斑岩钼矿SHRIMP锆石U—Pb和辉钼矿Re—Os年龄及其地质意义.地质学报,2006,780(7)：1078-1086
叶天竺,肖克炎,严光生.矿床模型综合地质信息预测技术研究.地学前缘,2007,14(5)：11-19
叶鑫.黑龙江省逊克县东安金矿矿床地质特征及成因研究：[硕士学位论文].长春：吉林大学,2011
尹冰川,冉清昌.小兴安岭—张广才岭地区区域成矿演化.矿床地质,1997,16(3)：235-242
于建波,苏仁奎,刘智明.东安金矿床控矿因素及成矿物质来源浅析.黄金科学技术,2005,13(6)：8-11
翟裕生,姚书振,林新多,等.长江中下游地区铁铜(金)成矿规律.北京：地质出版社,1992,1-234
翟裕生,姚书振,崔斌,等.成矿系列研究.武汉：中国地质大学出版社,1996：1-192
翟裕生,邓军,李晓波.区域成矿学.北京：地质出版社,1999
翟裕生.论成矿系统.地学前缘,1999,6(1)：13-28
翟裕生,吕古贤.构造动力体制转换与成矿作用.地球学报,2002,23(2)：97-102
翟裕生.成矿系统研究与找矿.地质调查与研究,2003,26(2)：65-72
翟裕生.地球系统科学与成矿学研究.地学前缘,2004,11(1)：1-10
张德会.流体的沸腾和混合在热液成矿中的意义.地球科学进展,1997,12(6)：546-552.
张海驲.黑龙江省印支期花岗岩的确定及其构造意义.黑龙江地质,1991,2(1)：8-18
张炯飞,李之彤,金成沫.中国东北部地区埃达克岩及其成矿意义.岩石学报,2004,20(2)：361-368
张理刚.稳定同位素在地质科学中的应用.西安：陕西科学技术出版社,1985,1-10
张旗,王焰,刘伟,等.埃达克岩的特征及其意义.地质通报,2002,21(7)：431-435
张旗,王焰,刘红涛,等.中国埃达克岩的时空分布及其形成背景.地学前缘,2003,10(4)：385-400
张旗,王焰,李承东等.花岗岩的Sr-Yb分类及其地质意义.岩石学报,2006,22：2249-2260
张旗,金惟俊,李承东,等.中国东部燕山期大规模岩浆活动与岩石圈减薄与大火成岩省的关系.地学前缘,2009,16(2)：21-51
张旗,李承东,等.花岗岩：地球动力学意义.北京：海洋出版社,2012,1-275
张苏江.黑龙江省铁力地区铝(铜)矿床成矿地质条件及找矿潜力分析：[硕士学位论文].长春：吉林大学,2009
张兴洲,杨宝俊,吴福元,等.中国兴蒙—吉黑地区岩石圈结构基本特征.中国地质,2006,33(4)：816-823.
张彦,陈文,陈克龙,刘新宇.成岩混层(I/S) Ar-Ar年龄谱型及39Ar核反冲丢失机理研究—以浙江长兴地区P-T界线粘土岩为例.地质论评,2006,52(4)：556-561
张昱.黑龙江省东部早中生代火成岩构造组合及其大地构造演化：[博士学位论文].北京：中国地质大学(北京),2008
张振庭.黑龙江省伊春地区铅锌多金属矿产预测：[硕士学位论文].长春：吉林大学,2010
张遵忠,吴昌志,顾连星,等.燕辽成矿带东段新台门钼矿床Re-Os同位素年龄及其地质意义.矿床地质,2009,28(3)：313-320
赵春荆,彭玉鲸,党增欣,等.吉黑东部构造格架及地壳演化.沈阳：辽宁大学出版社,1996
赵洪海,薛继广,连永牢.黑龙江省逊克县高松山矿区1号矿脉岩金详查报告.牡丹江：武警黄金第一总队,2011
赵鹏大,陈永清,刘吉平,等.地质异常成矿预测理论与实践.武汉：中国地质大学出版社,1999
赵一鸣,毕承思,邹晓秋,等.黑龙江多宝山铜山大型斑岩铜(铝)矿床中辉铝矿的铼—锇同位素年龄.地球化学,1997,18(1)：61-67
赵志丹,莫宣学,张双全等.西藏中部乌郁盆地碰撞后岩浆作用—特提斯洋壳俯冲再循环的证据.中国科学(D辑),2001,31(增刊)：20-26
周佐民.碱质A型花岗岩的判别、成因与构造环境.华南地质与矿产,2011,27(3)：216-220