| [1] | ［1］Berzina A N, Sotnikov V I,Ponomarchuk V A, et al. 1999. Temporal periods of formation of Cu-Mo porphyry deposits,Siberia and Mongolia [A]. In: Stanley C J, et al. ,eds. Mineral deposits: Processes toprocessing[C]. Rotterdam. 1: 321～324.
|
| [2] | ［2］Berzina A P, Sotnikov V I and Berzina A N. 1999. Porphyry Cu-Mo deposits andgeodynamic settings, Siberia, Mongolia [A]. In: Stanley C J, et al. ,eds. Mineraldeposits: Processes to processing[C]. Rotterdam. Balkema. 1: 317～320.
|
| [3] | ［3］Cunningham W D. 1998. Lithospheric controls on late Cenozoic construction of theMongolia Altai [J]. Tectonics, 17: 891～902.
|
| [4] | ［4］Du Q. 1988. Dtobaoshan porphyry copper deposits [M]. Beijing: Geol.Pub. House. 1～386(in Chinese).
|
| [5] | ［5］Gansu Bureau of Geology and Mineral Resources (GBGMR). 1989. Regional geology ofGansu Province [M]. Beijing: Geol. Pub. House.1～692 (in Chinese with English abstract).
|
| [6] | ［6］Gerel O. 1998. Phanerozoic felsic magratisnand related mineralization in Mongolia[J]. Bulletin of the Geological Survey of Japan, 49: 239～248.
|
| [7] | ［7］Hong D W, Wang S G, Xie X L, et al. 2000. Genesis of positive ε(Nd,t) granitoidsin the Da Hinggan Mrs-Mongolia orogenic belt and continental crustal growth [J]. EarthScience Frontiers, 7:441～456(in Chinese with English abstract).
|
| [8] | ［8］Hong D W, Wang S G, Xie X L, et al. 2003. Metallogenic province derived from mantlesource: a case studyof central Asian orogenic belt [J]. Mineral Deposits, 22(1): 41～55(in Chinese with English abstract).
|
| [9] | ［9］Huang C K, Bai Y, Zhu Y S, et al. 2001. Copper deposits of China [M]. Beijing:Geol. Pub. House. 1～371 (in Chinese).
|
| [10] | ［10］Inner Mongolian Bureau of Geology and Mineral Resources (IMBGMR).1991. Regionalgeology of Inner Mongolian Autonomrus Region [M]. Beijing: Geol. Pub. House. 1～725 (inChinese with English abstract).
|
| [11] | ［11］Lamb M A and Badarch G. 1997. Paleozoic sedimentary basins and volcanic-arcsystems of southern Mongolia: New stratigraphic and sedimentological constructions [J].Intemational Geology Review, 39:542～576.
|
| [12] | ［12］Lamb M A and Cox D. 1998. New 40Ar/39Ar age data and implications for porphyrycopper deposits of Mongolia [J]. Econ. Geol., 93:524～529.
|
| [13] | ［13］Li W S. 1997. Geology and genetic model of volcano-porphyry copperpolymetallicdeposits, southern Humeng[A]. In: Zhao Y M and Zhang D Q, eds. Metallogeny and prospectiveevaluation of copperpolymetallic deposits in the Da Hinggan Mountain and its adjacentregions [C]. Beijing: Seismological Press. 83～106 (in Chinese).
|
| [14] | ［14］Liu X Y and Wang Q. 1995. Tectonics of the orogenic belts in Beishan Mt., westernChina and their evolution [J]. Geological Research,28: 37～48 (in Chinese with Englishabstract).
|
| [15] | ［15］McMillan W J. 1992. Prophyry deposits in the Canadian cordillera ore deposit,tectonic-metallogeny in the Canadian cordillera [A].GeologicalSurvey of BritishColumbia-Paper 1991-4 [C]. Victoria:Queen\'s Printeer for British Columbia. 253～276.
|
| [16] | ［16］Nie F J, Zhang H T, Chen Q, et al. 1991. The zircon U-Pb age of metamorphosedbasic volcanic rocks from the Bainaimiao Group,Inner Mongolia [J]. Chinese ScienceBulletin, 36(9): 738～742.
|
| [17] | ［17］Nie F J, Pei R F, Wu L S, et al. 1993. Magmatic activity and metallogeny of theBainaimiao district, Inner Mongolia, People\'s Republic of China [M]. Beijing: Sci. &Tech. Press. 1～237 (in Chinese with English abstract).
|
| [18] | ［18］Nie F J, Pei R F, Wu L S, et al. 1994. Nd-Sr-Pb isotope study of Copper (gold) andgold deposits in Bainaimiao area, Inner Mongolia[J]. Mineral Deposits, 13 (4): 331～344(in Chinese with English alstract).
|
| [19] | ［19］Nie F J and Bj( )rlykke Ame. 1999. Nd and Sr isotope constraints on the age andorigin of Proterozoic meta-mafic volcanic rocks in BainaimiaoWenduermiao district, InnerMongolia, People\'s Republic of China [J]. Continental Dynamics, 4 (1): 1～14.
|
| [20] | ［20］Nie F J, Jiang S H and Zhao X M. 2000a. New advances on porphyry copper and golddeposits [J]. Geology of Inner Mongolia, (2): 1～11 (in Chinese with English abstract).
|
| [21] | 更多...
|
| [22] | ［21］Nie F J, Jiang S H and Zhao X M. 2000b. Ordovician intrusive-related Au-Cumineralization in central west New South Wales, Australia [J]. Acta Geologica Sinica,74(4): 807～826.
|
| [23] | ［22］Nie F J, Jiang S H, Bai D M, et al. 2002. Metallogeny and oreprospecting of oredeposits occurring within the conjunction area of Inner Mongolia, Gansu and Xinjiang(Beishan Mt. ), northwestern China [M]. Beijing: Geol. Pub. House. 1～499 (in Chinesewith English abstract).
|
| [24] | ［23］Perello J, Cox D, Garamjav D, et al. 2001. Oyu Tolgoi, Mongolia:Siluro-Devonianporphyry Cu-Au (Mo) and high-sulfidation Cu mineralization with a Cretaceous chalcociteblanket [J]. Econ. Geol. ,96: 1407～ 1428.
|
| [25] | ［24］Rui Z Y. 2000. Studies on the porphyry copper deposits of northwestem, northem andnortheastem China [A]. In: Tu G Z, ed. Superlarge mineral deposits [C]. Beijing: SciencePress. 397～ 425(in Chinese).
|
| [26] | ［25］Rui Z Y, Wang F T, Li H H, et al. 2001. Advance of the porphyry copper belt of theeastern Tianshan Mountain, Xinjiang[J]. Geology in China, 26 (2): 11～16 (in Chinese withEnglish abstract).
|
| [27] | ［26］Rui Z Y, Li Y L, Wang L S, et al. 2002. The eastern Tianshan porphyry copper beltin Xinjiang and its tectonic framework [J]. Acta Geologica Sinica, 76(1): 83～94 (inChinese with English abstract).
|
| [28] | ［27］Sheng J F and Fu X Z. 1997. Geology and genetic model of copper polymetallicdeposits, Tuquan-Tianshan district[A]. In: Zhao Y M and Zhang D Q, eds. Metallogeny andprospective evaluation of copperpolymetallic deposits in the Da Hinggan Mountains and itsadjacent regions [C]. Beijing: Seksnological Press. 107～124 (in Chinese).
|
| [29] | ［28］Tang K D. 1992. Tectonic evolution and minerogenetic regularities of the fold beltalong the northern margin of Sino-Korean plate [M]. Beijing: Peking University Press. 1～277(in Chinese with English abstract).
|
| [30] | ［29］Wang D W, Zou Z P and Li S X. 1995. On the ore-forming geological features and oredeposit genesis of the Gongpoquan copper deposit,Gansu province [J]. Northwest Geoscience,16(1): 115～122 (in Chinese with English abstract).
|
| [31] | ［30］Wang Q, Liu X Y and Li J Y. 1991. Plate tectonics between Cathaysia and Angaralandin China [M]. Beijing: Peking Unversity Press. 1～151 (in Chinese with English abstract).
|
| [32] | ［31］Wang Z T, Qin K Z and Zhang S L. 1994. Geology and exploration of large copperdeposits [M]. Beijing: Metallurgical Industry Press. 1～162 (in Chinese with Englishabstract).
|
| [33] | ［32］Watanabe Y and Stein H J. 2000. Re-Os ages for the Erdenet and Tsagaan Suvargaporphyry Cu-Mo deposits, Mongolia, and tectonic implications [J]. Econ. Geol. , 95:1537～1542.
|
| [34] | ［33］Xu Z G. 1997. Tectonic evolution and ore-controlling factors of the Da HingganMountains and its adjacent regions[A]. In: Zhao Y M and Zhang D Q, eds. Metallogeny andprospective evaluation of copperpolymetallic deposits in the Da Hinggan Mountains and itsadjacent regions [C]. Beijing: Seismological Press. 1～21(in Chinese).
|
| [35] | ［34］Yao ZQ, Zhang DQ and ZhaoY M. 1997. Geology and geneticrodek of the Duobaoshanlarge-scale porphyry copper deposit[A]. In: Zhao Y M and Zhang D Q, els. Metallogeny andprospective evaluation of copper-polymetallic deposits in the Da Hrmggan Mountains and itsadjacent regions [C]. Beijing: Seismological Press. 48～82 (in Chinese).
|
| [36] | ［35］Zhang Y, Nie F J and Jiang S H. 2003. Discovery of the Oyu Tolgoi porphyrycopper-gold deposits along the Sino-Mongolia border and its significance for furthermineral exploration [J]. Geological Bulletin of China, 22 (9): 708～712 (in Chinese withEnglish abstract).
|
| [37] | ［36］Zhao Y M, Bi C S, Zou X Q, et al. 1997. The Re-Os isotopic age of molybdenite fromDuobaoshan and Tongshan porphyry copper (molybdenum) deposits[J]. Acta Geoscientia Sinica,18(1): 61～67 (in Chinese with English abstract).
|
| [38] | ［37］Zhao Y Y, Ma Z H, Feng B Z, et al. 1997. Geochemical and prospecting studies ofthe Duobaoshan copper metallogenic system [M].Changchun: Jilin People\'s Press. 1～155 (inChinese).
|
| [39] | ［38］杜琦.1988.多宝山斑岩铜矿床[M].北京:地质出版社.1～386.
|
| [40] | 洪大卫,王试光,谢锡林,等2003.试析地幔来源物质成矿域[J].矿床地质,22(1):41-55.
|
| [41] | ［42］黄崇轲,白冶,朱裕生,等2001.中国铜矿床(上册)[M].北京:地质出版社.1～371.
|
| [42] | ［43］李伟实1997.呼盟南部浅火山-斑岩铜多金属矿床地质及成矿模式[A].见:张德全,赵一鸣,主编.大兴安岭及邻区铜多金属矿床论文集[C].北京:地震出版社.83～106.
|
| [43] | ［44］刘雪亚,王荃.1995.中国西部北山造山带的大地构造及其演化[J].地学研究,(28):37～48.
|
| [44] | ［45］内蒙古自治区地质矿产局.1991.内蒙古自治区区域地质志[M].北京:地质出版社.1725.
|
| [45] | ［46］聂凤军,裴荣富,吴良士,等.1993.内蒙古白乃庙地区岩浆活动与金属成矿作用[M].北京:北京科学技术出版社.1～239.
|
| [46] | ［47］聂凤军,裴荣富,吴良士,等.1994.内蒙古白乃庙地区铜(金)矿床钕、锶和铅同位素研究[J].矿床地质,13(4):331～344.
|
| [47] | ［48］聂凤军,江思宏,赵省民.2000a.斑岩型铜金矿床研究新进展[J].内蒙古地质,2(总第95期):1～11.
|
| [48] | ［49］聂凤军,江思宏,白大明,等.2002.北山地区金属矿床成矿规律及找矿方向[M].北京:地质出版社.1499.
|
| [49] | ［50］芮宗瑶.2000.西北、华北、东北斑岩铜矿床研究[A].见涂光炽等著.中国超大型矿床[C].北京:科学出版社.397～425.
|
| [50] | ［51］芮宗瑶,王福同,李恒海,等.2001.新疆东天山斑岩铜矿带的新进展[J].中国地质,28(2):11～16.
|
| [51] | ［52］芮宗瑶,刘玉琳,王龙生,等.2002.新疆东天山斑岩铜矿带及其大地构造格局[J].地质学报,76(1):83～94.
|
| [52] | ［53］盛继福,付先政.1997.突泉-天山地区铜多金属矿床地质及成矿模式[A].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[C].北京:地震出版社.107～124.
|
| [53] | ［54］唐克东.1992.中朝板块北侧褶皱带构造演化及成矿规律[M].北京:北京大学出版社.1～277.
|
| [54] | ［55］王荃,刘雪亚,李锦轶.1991.中国华夏与安加拉古陆间的板块构造[M].北京:北京大学出版社.1～151.
|
| [55] | ［56］王大为,邹治平,李绍雄.1995.甘肃公婆泉铜矿成矿地质特征及矿床成因[J].西北地质科学,16(1):115～122.
|
| [56] | ［57］王之田,秦克章,张守林.1994.大型铜矿地质与找矿[M].北京:冶金工业出版社.1～162.
|
| [57] | ［58］徐志刚.1997.大兴安岭及其邻区构造演化及控矿作用[A].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[C].北京:地震出版社.1～21.
|
| [58] | ［59］姚志强,张德全,赵玉明.1997.多宝山大型斑岩铜矿地质及成矿模式[A].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[C].北京:地震出版社.48～82.
|
| [59] | ［60］张义,聂凤军,江思宏.2003.中蒙边境欧玉陶勒盖大型铜-金矿床的发现及对找矿勘查工作的启示[J].地质通报,22(9):708～712.
|
| [60] | 赵一鸣,毕承思,邹晓秋.1997.黑龙江多宝山,铜山大型斑岩铜(钼)矿床中辉钼矿的铼-锇同位素年龄[J].地球学报,18(1):61～67.
|
| [61] | ［39］甘肃省地质矿产局1989.甘肃省区域地质志[M].北京:地质出版社.1～692.
|
| [62] | ［40］洪大卫,王试光,谢锡林,等.2000.兴蒙造山带正ε(Nd,t)值花岗岩的成因和大陆地壳生长[J].地学前缘,7(2):441～456.
|
| [63] | ［62］赵元艺,马志红,冯本智,等.1997.多宝山铜矿床系统地球化学及找矿研究[M].长春:吉林人民出版社1～155
|
