参考文献

如题所述

曹永清.1999.东昆仑—柴达木盆地北缘岩浆活动、构造演化、深部过程与成矿(博士学位论文),中国地质大学(北京),1~91

常承法,潘裕生,郑锡澜等.1982.青海高原地质构造.北京:科学出版社,20~60

常印佛,刘湘培,吴言昌.1991.长江中下游铜铁成矿带.北京:地质出版社,1~379

陈义贤,陈文寄,周新华等.1991.辽西及邻区中生代火山岩.北京:地震出版社,1~279

陈义贤,陈文寄,周新华等.1997.辽西及邻区中生代火山岩.北京:地质出版社,1~279

陈毓川主编.1999.中国主要成矿区带矿产资源远景评价.北京:地质出版社,1~536

池际尚,路凤香主编.1996.华北地台金伯利岩及古生代岩石圈特征.北京:科学出版社,1~292

邓晋福,戴圣潜,赵海玲等.2002c.铜陵Cu-Au(Ag)矿床——流体-成矿系统和亚系统的识别.矿床地质,21(4):317~322

邓晋福,鄂莫岚,路风香.1985.东北地质新生代玄武岩及其与大陆裂谷构造的关系.见:国际交流地质学术论文集——为27届国际地质大会撰写,第3号.北京:地质出版社,13~22

邓晋福,赖绍聪,赵海玲等.1994.青海陆内造山火成岩成对性与造山过程[A].见:欧阳自远,中国矿物岩石地球化学研究新进展(1)[C].兰州大学出版社,134~135

邓晋福,刘厚祥,赵海玲等.1996.燕辽地质燕山期火成岩与造山模型.现代地质,10(2),137~148

邓晋福,莫宣学,罗照华等.1999.火成岩构造组合与壳幔成矿系统.地学前缘,6(2):259~269

邓晋福,莫宣学,罗照华等.2001.青藏高原岩石圈不均一性及其动力学意义.中国科学(D),31(增刊):55~60

邓晋福,莫宣学,肖庆辉等.2002b.地质事件序列与造山过程PTt轨迹.岩石矿物学杂志,21(4):336~342

邓晋福,莫宣学,赵海玲等.1997.新生代以来中国大陆岩石圈尺度的大地构造分区.地球科学,22(3):227~232

邓晋福,莫宣学,赵海玲等.1997.岩浆活动与地球多层对流系统.地学前缘,4(3~4):205~210

邓晋福,莫宣学,赵海玲等.1998a.壳幔物质与深部过程.地学前缘,5(3):67~75

邓晋福,莫宣学,赵海玲等.1999b.岩石圈/软流圈系统的大灾害与巨型矿集区形成.见:裴荣富,翟裕生,张来红主编,深部构造作用与成矿.北京:地质出版社,36~43

邓晋福,莫宣学,赵海玲等.1999c.中国岩石圈-软流圈系统大灾害与成矿环境.矿床地质,18(4):309~315

邓晋福,吴宗絮.2001.下扬子克拉通岩石圈减薄事件与长江中下游Cu-Fe成矿带.安徽地质,11(2):86~91

邓晋福,杨建军,赖绍聪等.1996b.格尔木-额济纳旗断面走廊火成岩构造组合和大地构造演化.现代地质,10(3),330~343

邓晋福,叶德隆,赵海玲等.1992.下扬子地质火山作用、深部过程与盆地形成.武汉:中国地质大学出版社,1~184

邓晋福,赵崇贺.1996a.华北地台的构造格局及其与金伯利岩岩浆活动的关系.见:池际尚,路风香主编:华北地台的金伯利岩及古生代岩石圈地幔特征[C].北京:科学出版社,1989,7~15

邓晋福,赵崇贺等.1980.武山含矿(铜)岩体的岩石学及其成因探讨.矿物学岩石学论丛(一).北京:地质出版社,14~89

邓晋福,赵海玲,莫宣学等.1996a.中国大陆根-柱构造.北京:地质出版社,1~110

邓晋福,戴圣潜,吴宗絮等.2000a.大别造山带岩石学结构和热结构及其地质意义.地质学报,74(3):206~215

邓晋福,莫宣学,赵海玲等.1994.中国东部岩石圈根/去根作用于大陆活化.现代地质,8(3):349~356

邓晋福,汪洋,赵海玲等.2002a.岩浆-构造-热事件序列PTt轨迹与造山深部过程.见:肖庆辉等花岗岩研究思维与方法.北京:地质出版社,121~127

邓晋福,吴宗絮,莫宣学等.1999a.华北地台前寒武花岗岩类、陆壳演化与克拉通形成.岩石学报,15(2):190~198

邓晋福,赵海玲,罗照华等.1998.岩石圈软流圈系统的形成与演化[A].见:欧阳自远主编,世纪之交矿物学岩石学地球化学的回顾与展望[ C].北京:原子能出版社,97~104

邓晋福.1987.岩石相平衡与岩石成因.武汉:武汉地质学院出版社,1~198

邓晋福.1989.开放的岩浆体系八十年代火成岩研究的新进展之一.地质科技情报,8(2):1~7

邓晋福.1990.岩浆-成矿作用-板块构造.地质科技情报,9(2):39~44

洪大卫,王式洗,黄怀曾.1991.中国北疆及其邻区晚古生代—三叠纪碱性花岗岩带及其地球动力学意义初探,见:中国北方花岗岩及其成矿作用论文集.北京:地质出版社,40~48

洪大卫等.2000.兴蒙造山带正(Nd,t)值花岗岩的成因和大陆地壳生长.地学前缘,7(2):441~456

赖绍聪,刘池阳,Oreilly S R.2001.北羌塘高钾钙碱火山燕系列成因及其大陆动力学意义.中国科学(D),31(增刊):34~42

李文达,毛建红,朱云鹤等.1996.中国东南部中生代火成岩与矿床.北京:地震出版社,1~157

罗照华,邓晋福,曹永清等.1999.青海省东昆仑地质晚古生代—早中生代火山活动的区域构造演化.现代地质,13(1):51~56

莫宣学、路风香、沈上越等.1993.三江特提斯火成作用与成矿.北京:地质出版社

潘桂棠,王培生,徐耀荣等.1990.青藏高原新生代构造演化.北京:地质出版社,6~24

裴荣富,吴良士,熊群尧等.1998.中国特大型矿床成矿偏在性与异常成矿构造聚敛场.北京:地质出版社,1~418

邱瑞照,邓晋福,周肃等.2004.华北地区岩石圈类型:地质与地球物理证据[J].中国科学(D辑),34(8):689~711

任纪舜,王作勋,陈炳蔚等.1999.中国及邻区大地构造图及其说明书.北京:地质出版社,1~50

汤中立,李文渊.1995.金川铜镍(含硫)矿床成矿模式及地质对比.北京:地质出版社,1~209

唐永成,吴宗昌,储国正等.1998.安徽沿江铜金属矿床地质.北京:地质出版社,1~351

涂光炽.1998.试论非常规超大型矿床物质组成、地质背景、形成机制的某些独特性.中国科学(D辑),28(增刊):1~6

涂光炽等.2000.中国超大型矿床(Ⅰ).北京:科学出版社,1~584

涂光炽主编.1995.庞然大物-与寻找超大型矿床有关的基础研究.长沙:湖南科学技术出版社,1~116

韦永福,吕英杰.1994.中国金矿床.北京:地震出版社,379

吴福元,江博明,林强.1997.中国北方造山带造山后花岗岩的同位素特点与地壳生长意义.科学通报,42:2188~2192

吴宗絮.1985.华南其些含稀土元素花岗岩的地球化学特征及其形成的物理化学条件.岩石学报,1(1):34~48

肖序常,李廷栋.2000.青藏高原的构造演化与隆升机制.广州:广东科技出版社,1~313

翟裕生,邓军,李小波.1999.区域成矿学.北京:地质出版社,1~287

翟裕生,姚书振,林新多等.1992.长江中下游铁铜(金)成矿规律.北京:地质出版社

翟裕生,张湖,宋鸿林等.1997.大型构造与超大型矿床.北京:地质出版社,1~180

翟裕生.1997.地史中成矿演化的趋势和阶段性.地学前缘,4(4):197~204

张理刚.1994.东亚岩石圈块体地质.北京:科学出版社,1~379

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:地质出版社,1~318

Boyd FR.1989.Compositional distinction between oceanic and cratonic lithosphere.EPSL 96:15~26

Condie K.C.Plate tectonics and crustal evolution.New York:Pergamon,1982:1~310

Davis G A,Qian X-L,Zheng Y-D et al.1996.Mesozoic deformation and plutouism in the Yunmeng Shan:a metamorphic core complex noreh of Beijing,China.In:Yin A.&Harrison TM eds.The tectonic evolution of Asia,Carmb.Univ.Press.253~280

Davis GA,Zheng YD,Wang C et al.,2001.Mesozoic tectonic evolution of the Yanshan fold and thrust belt,with emphsis on He-bei and Liaoning provinces,northern China,GSA,Memoir 194,171~197

Deng Jinfu,Luo Zhaohua,Zhao Hailing,et al.1998.Trachyte and syenite:petrogenesis constrained by the petrological phase e-quilibrium.北京大学国际地质科学学术研讨会论文集.北京:地质出版社,745~757

England P C & Thompson A B.1986.Some thermal and tectonic models for crustal meleting in continental collision zones[A].Coward & Ries.Collision Tectonics[ C],GSA Spec.Pub.,19:83~94

Falloon T J&Danyushebsky L V.2000.Melting of rafractory mantle at 1.5,2and 2.5 Gpa under anhydrous and H2 O-undersatu-rated condition:Implications for the petrogenesis of high-Ca boninites and the influence of subduction components on mantle meltong,H.Petrol.,41(2):257~283

Flower M F J,Tamaki K&Hoang N.1998.Mantle extrusion:A model for dispersed volcanism and DUPAL-like asthenosphere in east Asia and the westera Pacific.In Flower et al eds,Mantle plane and plate interactions in East Asia,Geodyn.series,27,AGU,Washington,67~88

Flower,MFJ,Russo RM,Widom E et al.2000.The significance of boninite in Tethyan subduction-accretion complexes,IGCP-430 workshop I,Civasna Romania,Abstract,20~22

Frey FA 1978,Intergrated models of basaltic petrogenesis:A study of quartzw tholeiite to olivine melilite from south eastern Aus-tralia utilaizing geochemical and experimental petrological data,J.Petrol.19:463~513

Gee L L & Sack RO,1988,Experimental petrology of melilite nephilinites,J.Petrol,29:1233~1255

Gill JB.1981.Orogenic andesites and plate tectonics,New York:Springer-Verlag,390

Grovew TL&Kinzler RJ,1986.Petrogenesis of andesites,Ann.Rev.Earth Plant.Sci.,14:417~454

Huang X,Ziwei B and DePaolo.1986.Sm-Nd isotope study of early Archean rocks.Qiannan,Hebei Province,China.Geochim.Cosmochim.Acta,50:625~631

Jahn B M,Zhou XH,Li JL.1990.Formation and tectonic evolution of southeadtern China and Taiwan:Isotopic and geochemical constraints.Tectonophys.183:145~160

Jahn BM,Vidal P,Kroner A.1984.Multi-chronometric ages and origin of Archaean tonalitic genisses in Finnish Lapland:a case for ling crustal residence time.Contrib,Mineral Petrol.,86:398~408

Jin Wei and Lin Shuxun.1994.The lithological association and geological features of early Proterozoic orogenic belt Daqinshan,Nei Mongol,in:Qian X andWand R.eds.Geological evolution of the gramulite terrain in north part of the north China cra-ton.Beijing:Seismol.Press,32~42(in Chinese with English abstract)

Johnston A D and Wyllie P J.1988.Constraints on the origin of Archean trondhjimites based on phase relationships of Nuk gneiss with H2 Oat 15kbar.Contrib.Mineral.Petrol.,100:35~46

Kushirn I,1990.Partial melting of mantle wedge and evolution of island arc crust,JGR 95(B10)15929~15939

Le Fort P.1981.Manashi leucogranite:a collision signature of the Himalaya,a model for it genesis and emplacement,JGR,86(B11):10545~10568

Liegeois J-P,Navez J,Hertogen J et al.1998.Contrasting origin of post-collisional high-k calc-alkaline and shoshonitic versus al-kaline and peralaline granitoids.The use of sliding normalization.Lithos,45:1~28

Lu Liangzhao,Xu Xuechun and Lin Fula.1996.Early Precambrian khondalite serier in north part of China.Zhangchun:Zhang-chun Press.1~276

Martin H.1987.Petrogenesis of Archean Trondhjemitesn tonalities and granodiorites from eastern Finland:major and trace ele-ment geochemistry.J.Petrol.28:921~953

Morgan P.1984.The thermal structure and thermal evolution of the continental lithosphere.Phys.Chem.Earth,15:107~193

Morrison G W.1980.Characteristics and tectonic setting of the shoshonite rock association.Lithos,13:97~108

Mysen B.1975.Partitioning of iron and magnesium between crystals and partial melts in peridotite upper mantle.CMP,52:69~76

Oliver J.1986.Fluids expelled tectonically from orogenic belts:Their role in hydrocarbon migration and other geologic phenomena Geol.14:99~102

Pan Y,Kidd W S F.1992.Nyainqentanglha shear zone:Alate Miocene extensional detachment in the southern Tibetan Plateau.Geol.,20:775~778

Pei Rongfu & Hong Dawei.The granite of south China and their metallogeny.Episodes,1995,18(1~2):77~82

Polet J&Anderson D L.1995.Septh estent of cratous as inferred from tomograpohic studies Geol.,23:205~208

Qian Xianglin and Wang Renmin et al.1994.Geological evolution of the granulite terrain in north China craton.Seismol.Press.1~234

Rapp RP,Watson E B,Miller C F.1991.Partial melting of amphibolite/eclogite and the origin of Archean trindhjemites and to-nalites,Precamb.Res.,51:1~25

Ringwood AE.1975.Composition and petrology of the Earth’s mantle,McGraw-Hill,Inc.1~618

Sun Dazhong and Wu Weixing et al.1993.Precamlrian age-tectonic framework and age-crustalstucture of Zhongtiao Shan,Bejing:Geol.Pub.house,1~180

Sun Weiton,Ben Zichang and Zhi Xianchang et al.1997.Os-isotopic composition of peridotite xenolith in Panshishan by N-TIMS method.Chinese Sci.Bull.42(21):2310~2313

Sylvester PJ.1989.Post-collisional alkaline granites.J.Geol.,97:261~280

Takahashi E&Kushino I.1983.Melting if a dry peridotite at high pressure and basbaltic magma genesis,Am,Miner.68:859~879

Thomposon A B&England PC.1984.Pressure-temperature-time paths of regional metamorphism.Ⅱ,Their inference and inter-pretation fron using mineral assemblages in metamorphic rocks.J.Petrol.,25(4):929~955

Tu Guangzhi.1995.Some problems pertaining to super-large ore deposits of China.Episodes,116

Wang Hongzheng,MoXuanxue.1995.An outline of the tectonic evolution of China.Episodes,18(1~2):6~16

Zhai YS,Deng J.1996.Outline of the mineral reaources of China and their tectonic setting.Austral.J.Earth Sci.,43:673~685

温馨提示:答案为网友推荐,仅供参考
第1个回答  2020-04-27
相似回答