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矿床地质  2003 

试析地幔来源物质成矿域——以中亚造山带为例

Keywords: 地质学,成矿物质来源,成矿域,中亚造山带,综述

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Abstract:

文章总结了大量的Sr,Nd,S,Pb多元同位素资料,据此认为,中亚造山带的铜、金多金属矿床与区域花岗岩在形成时代和物质来源上基本吻合,具有一定的继承性。从古生代直至中生代,地幔来源物质参与了成岩成矿作用,即便是钨、锡、稀有金属矿床,也受到地幔来源物质的明显影响,从而揭示了地幔来源物质在中亚造山带金属成矿作用中的重要意义。

References

[1]  [39]Sotnikov V I, Ponomarchuk V A, Berzina A P, et al. 1995. Geochronological borders of magmatism of Cu-Mo porphyry Erdenetuin-Obo deposit (Mongolia)[J]. Geol. & Geophys., 36(3): 78~89(in Russian).
[2]  [40]Tu G Z. 1999. On the central Asia metallogenic province[J], Sci. Geol. Sinica, 34(4): 397~404(in Chinese with English abstract).
[3]  [41]Veevers J J. 1994. Pangea: evolution of a supercontinent and its consequences for Earth\'s paleoclimate and sedimentary environments[A]. In: Klein G D, ed. Pangea, paleoclimate, tectonics, and sedimentation during accretion, zenith, and breakup of a supercontinent, Boulder, Colorado[C]. Geol.Soc.Am.Spec., Paper 288: 13~23.
[4]  [42]Vladimirov A G, Ponomareva A P, Shokalskii S P, et al. 1997. Late Paleozoic-early Mesozoic granitoid magmatism in Altai[J]. Geol. & Geophys., 38(4): 715~729 (in Russian).
[5]  [43]Vladimirov A G, Vystavnoi S A, Titov A V, et al. 1998. Petrology of the early Mesozoic rare-metal granites of the southern Gorng Altai[J]. Geol. & Geophys., 39(7): 901~916 (in Russian).
[6]  [44]Wang D H, Chen Y C, Xu Z G, et al. 2002. Metallogenic series and metallogeny in the Altai metallogenic province[M]. Beijing: Atomic Power Press. 493p (in Chinese).
[7]  [45]Wang G Z. 1997. Geological characteristics and genesis of the Anle tin-copper deposit, Inner Mongolia[J]. Mineral Deposits. 17(3): 260~271(in Chinese with English abstract).
[8]  [46]Wang Y X and Zhao Z H. 1997. Geochemistry and origin of the Baerzhe REE-Nb-Be-Zr superlarge deposit [J]. Geochemistry, 26(1): 24~35(in Chinese with English abstract).
[9]  [47]Wang Z G, Zhao Z H, Zhou T R, et al. 1998. Geochemistry of the granitoids in Altai [M]. Beijing: Sci. Press. 152p(in Chinese).
[10]  [48]Wu F Y, Sun D G and Lin Q. 1999. Petrogenesis of the Phanerozoic granites and crustal growth in northeast China[J]. Acta Petrol. Sinica, 15(2): 181~189(in Chinese with English abstract).
[11]  [49]Xiang W D, Hu S K, Yan H Q, et al. 1998. Metallogenic significance of the Mesozoic volcanic magmatism in the western slope of Da Hinggan Mountains and its adjacent area[J]. Mineral Deposits, 17(supp.): 67~70(in Chinese).
[12]  [50]Ye Q T, Wu Y P, Fu X J, et al. 1999. metallogenic condition and prospecting of nonferrous metallic deposits in southwest Tianshan mountains[M]. Beijing: Geol. Pub. House. 201p(in Chinese with English abstract).
[13]  [51]Zartman R E and Doe B R. 1981. Plumbotectonics:the model[A]. In: Zartman R E and Taylor S R, ed. Evolution of the upper mantle[C]. Tectonophysics, 75: 135~162.
[14]  [52]Zhang D Q. 1993. Two granitoid series in different tectonic environments of southern Da Hinggan Mountains, China[J]. Acta Petrol. et Mineral. 45(1): 1~11(in Chinese with English abstract).
[15]  [53]Zhang Q F, Hu A Q, Zhang G X, et al. 1994. Evidence from isotopic age for presence of Mesozoic-Cenozoic magmatic activities in Altai region, Xinjiang[J]. Geochemistry, 23(3): 269~279(in Chinese with English abstract).
[16]  [54]Zhao Y L, Ma Z H, Feng B Z, et al. 1997. Geochemical and prospecting study of the Duobaoshan copper metallogenic system[M]. Jilin: Jilin People\'s Press. 155p(in Chinese).
[17]  [55]Zhao Y M and Zhang D Q. 1997. Metallogeny and prospective evaluation of copper-polymetallic deposits in the Da Hinggan Mountains and its adjacent regions[M]. Beijing: Seismol. Press. 318p(in Chinese with English abstract).
[18]  [56]Zhou G, Han D N and Deng J N. 1998. Study of isotope geochemistry on the Keketale Lead-Zinc deposit, Xinjiang[J]. Min. Res. & Geol., 12(1): 33~38(in Chinesewith English abstract).
[19]  [57]Zhou G, Qin J H, He L X, et al. 1999. Formation time of granitoids in Sawuer Mountains, Xinjiang[J]. Acta Petrol. et Mineral., 18(3): 237~242(in Chinese with English abstract).
[20]  [58]Zhu Y F, Sun Z H and Jiang N. 2001. A gold-bearing alkaline pluton in eastern Linxi district, Inner Mongolia: Its geochemistry and metallogenic significance[J]. Resource Geol., 51(4): 393~399.
[21]  [59]毕承思, 沈湘元, 徐庆生, 等. 1993. 新疆贝勒库都克锡矿带含锡花岗岩地质特征[J]. 岩石矿物学杂志, 12(3): 213~223.
[22]  陈德潜, 赵平, 魏振国. 1995. 论小坝梁铜矿床的海底火山热液成因[J]. 地球学报, (2): 190-203.
[23]  [61]陈富文, 李华芹, 蔡红, 等. 1999. 新疆干梁子锡矿田成岩成矿作用同位素年代学研究及矿床成因探讨[J]. 矿床地质, 18(1): 91~97.
[24]  [62]陈富文, 李华芹, 王登红, 等. 1999. 中国阿尔泰造山带燕山期成岩成矿同位素年代学新证据[J]. 科学通报, 44(11): 1142~1148.
[25]  [63]戴自希, 白冶, 吴初国, 等. 2001. 中国西部和毗邻国家铜金找矿潜力的对比研究[M]. 北京: 地震出版社. 201页.
[26]  [70]聂凤军, 江思宏. 2000. 中蒙边境塔林大型金矿化带发现对我们的启示[J]. 内蒙古地质, (2): 20~23.
[27]  [71]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. 239页.
[28]  秦克章. 1998. 额尔古纳南段中生代斑岩-次火山岩-浅成低温Cu,Mo,Pb,Zn,Ag成矿系统[J]. 矿床地质, 17(增刊): 201-206.
[29]  [73]芮宗瑶, 刘玉琳, 王龙生, 等. 2002. 新疆东天山斑岩型铜矿带及其大地构造格局[J]. 地质学报, 76(1): 83~94.
[30]  [74]盛继福, 付先政. 1999. 大兴安岭中段成矿环境与铜多金属矿床地质特征[M]. 北京: 地震出版社. 216页.
[31]  [75]盛继福, 李岩, 王湘云, 等. 1993. 内蒙古布敦化铜矿床地质特征及成矿作用[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. 116~125.
[32]  [76]宋叔和. 1992. 中国矿产资源图1∶5000 000[M]. 北京: 地质出版社.
[33]  [1]Bates R L and Jackson J A. 1987. Glossary of geology[M]. 3nd ed. Virginia: American Geological Institute, Falls Church. 788p.
[34]  [2]Bi C S, Shen X Y, Xu Q S, et al. 1993. Geological characteristics of stanniferous granites in the Beilekuduk tin metallogenic belt, Xingjiang[J]. Acta Petrol. and Mineral., 12(3): 213~223(in Chinese with English abstract).
[35]  [3]Bowring S A and Housh T. 1995. The earth\'s early evolution[J]. Sci., 269: 1535~1540.
[36]  [4]Chen D Q, Zhao P and Wei Z G. 1995. On the submarine volcanic hydrothemal genesis of the Xiaobaliang copper deposit[J]. Acta Geosci. Sinica, (2): 190~203(in Chinese with English abstract).
[37]  [5]Chen F W, Li H Q, Wang D H, et al. 1999a. New chronological evidence of the Mesozoic rock-forming and metallogenic events in the Altay orogenic belt, China[J].. Chinese Sci. Bull., 44(11): 1142~1148(in Chinese with English abstract).
[38]  [6]Chen F W, Li H Q, Cai H, et al. 1999b. Chronology and origin of the Ganliangzi tin orefield, Xinjiang[J]. Mineral Deposits, 18(1): 91~97(in Chinese with English abstract).
[39]  [7]Chu X L, Huo W G and Zhang X. 2001. Sulfur, carbon and lead isotope studies of the Dajing polymetallic deposit in Linxi County, Inner Mongolia, China:Implication for metallogenic elements from hypomagmatic source[J]. Res. Geol., 51(4): 333~344.
[40]  [8]Dai Z X, Bei Y, Wu C G, et al. 2001. Comparision of metallogenic potentiality between western China and its adjacent countries[M]. Beijing: Seismol. Press. 201p(in Chinese).
[41]  [9]De Paolo D J. 1981. A Nd and Sr isotopic study of the Mesozoic cale-alkaline granitic batholiths of the Sierra Nevada and Peninsular Ranges, California[J]. J. Geophys. Res., 86: 10470~10488.
[42]  [10]Dobretsov N L, Berzin N A and Buslov M M. 1995. Opening and tectonic evolution of the Paleo-Asian ocean[J]. International Geol. Rev., 37: 335~360.
[43]  [11]Doe B R and Zartman R E. 1979. Plumbotectonics, the Phanerozoic[A]. In: Barnes HL ed. Geochemistry of hydrothermal ore deposits[C]. 2nd edition. New York: John Wiley and Sons. 22~70.
[44]  [12]Du Q. 1988. Doubaoshan porphyry copper deposits[M]. Beijing: Geol. Pub. House. 386p(in Chinese).
[45]  [34]Qin K Z. 1998. The Mesozoic porphyry-subvolcanic-epithermal Cu, Mo, Pb. Zn, Ag metallogenic systematics in southern Ergun[J]. Mineral Deposits, 17(supp.): 201~206(in Chinese).
[46]  [35]Rui Z Y, Liu Y L, Wang L Z, et al. 2002. The eastern Tianshan porphyry copper belt in Xinjiang and its tectonic framework[J]. Acta Geol. Sinica, 76(1): 83~94(in Chinese with English abstract).
[47]  [36]Sheng J F and Fu X Z. 1999. Metallogenic settings and geological characteristics of the copper polymetallic deposits in the middle segment of Da Hinggan Mountains[M]. Beijng: Seismol. Press. 216p(in Chinese).
[48]  [37]Sheng J F, Li Y, Wang X Y, et al. 1993. Geological characteristics and metallogeny of the Budenghua copper deposits, Inner Mongolia [A]. In Zhang D Q and Zhao Y M, ed. Contritutions to the copper-polymetallic deposits in the Da Hinggan Mountains and its adjacent regions[C]. Beijng: Seismol. Press. 116~125(in Chinese with English abstract).
[49]  [38]Song S H. 1992. Mineral Resources Map of China, 1∶ 5000000[M]. Beijing: Geol.Pub. House(in Chinese).
[50]  [77]涂光炽. 1999. 初议中亚成矿域[J]. 地质科学, 34(4): 397~404.
[51]  [78]王登红, 陈毓川, 徐志刚, 等. 2002. 阿尔泰成矿省的成矿系列及成矿规律[M]. 北京: 原子能出版社. 493页.
[52]  [79]王国政. 1997. 内蒙古安乐锡铜矿床地质特征及成因[J]. 矿床地质, 16(3): 260~271.
[53]  [80]王一先, 赵振华. 1997. 巴尔哲超大型稀土铌铍锆矿床地球化学和成因[J]. 地球化学, 26(1): 24~35.
[54]  [81]王中刚, 赵振华, 邹天人, 等. 1998. 阿尔泰花岗岩类地球化学[M]. 北京: 科学出版社. 152页.
[55]  [82]吴福元, 孙德有, 林强. 1999. 东北地区显生宙花岗岩的成因与地壳增生[J]. 岩石学报, 15(2): 181~189.
[56]  向伟东, 胡绍康, 阎鸿铨, 等. 1998. 大兴安岭西坡及邻区中生代火山岩浆作用的成矿意义[J]. 矿床地质, 17(增刊): 67-70.
[57]  [84]叶庆同, 吴一平, 傅旭杰, 等. 1999. 西南天山有色金属矿床成矿条件和成矿预测[M]. 北京: 地质出版社. 201页.
[58]  [85]张德全. 1993.大兴安岭南段不同构造环境中的两类花岗岩[J]. 岩石矿物学杂志, 12(1): 1~11.
[59]  [86]张前锋, 胡霭琴, 张国新, 等. 1994. 阿尔泰地区中、新生代岩浆活动的同位素年龄证据[J]. 地球化学, 23(3): 269~279.
[60]  [87]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[M]. 北京: 地震出版社. 318页.
[61]  [88]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. 155页.
[62]  [89]周刚, 韩东南, 邓吉牛. 1998. 新疆可可塔勒铅锌矿床同位素地球化学研究[J]. 矿产与地质, 12(1): 33~38.
[63]  [90]周刚, 秦纪华, 何立新, 等. 1999. 新疆萨吾尔山花岗岩类的形成时代[J]. 岩石矿物学杂志, 18(3): 237~242.
[64]  [13]He B C, Tan K R and Wu Q H. 1994. Ages and Sr, Nd isotopic evidences of mantle source magmatite in the Bu\'s gold deposit, Jimunai County, northern Xinjiang[J].. Geotectonica et Metallogenia, 18(3): 219~228 (in Chinese with English abstract).
[65]  [14]Heinhorst J, Lehmann B, Ermolov P, et al. 2000. Paleozoic crustal growth and metallogeny of Central Asia: evidence from magmatic-hydrothermal ore systems of Central Kazakhstan [J]. Tectonophysics, 328: 69~87.
[66]  [15]Hildreth W and Moorbath S. 1998. Crustal contribution to arc magmatism in the Andes of Central Chile [J]. Contrib. Miner. Petrol., 98: 455~489.
[67]  [16]Hong D W, Huang H Z, Xiao Y J, et al. 1994. The Permian alkaline granites in central Inner Mongolia and their geodynamic significance [J]. Acta Geol. Sinica, 68(3): 217~230(in Chinese with English abstract).
[68]  [17]Hong D W, Wang S G, Xie X L, et al. 2000. Genesis of positive εNd granitoids in the Da Hinggan Mts-Mongolia oroganic belt and continental crustal growth[J]. Earth Sci. Frontiers, 7: 441~456 (in Chinese with English abstract).
[69]  [18]Hong D W, Xie X L and Zhang J S. 1998. Isotope geochemistry of granitoids in south China and their Metallogeny[J]. Res. Geol., 48: 251~263.
[70]  [19]Jahn B M, Wu F and Hong D. 2000a. Important crustal growth in the Phanerozoic: Isotopic evidence of granitoids from east-central Asia[J]. Proc.Indian Acad.Sci..(Earth Planet Sci.), 109(1): 5~20.
[71]  [20]Jahn B M, Wu F and Chen B. 2000b. Masssive granitoid generation in central Asia: Nd isotopic evidence and implication for continental growth in the Phanerozoic[J]. Episodes, 23: 82~92.
[72]  更多...
[73]  [21]Ji J S, Tao H X,Yang X K, et al. 1994. Geology and metallogeny of the Kangguertage gold deposits, eastern Tianshan mountains[M]. Beijing: Geol. Pub. House. 200p(in Chinese).
[74]  [22]Khain E V, Bibikova E V, Kroner A, et al. 2002. The most ancient ophiolite of the Central Asian fold belt: U-Pb and Pb-Pb zircon ages for the Dunzhugur Comples, Eastern Sayan, Siberia, and geodynamic implications [J]. Earth Planet. Sci. Lett., 199: 311~325.
[75]  [23]Kovalenko V I, Thareva G M, Yarmolyuk V V, et al. 1992. Sr and Nd isotopic composition and ages of rare-metal bearing alkaline granitoids in western Mongolia[J]. Rep. Acad. Sci., 327: 570~754(in Russian).
[76]  [24]Kovalenko V I, Yarmolyuk V V, Kovach V P, et al. 1996. Sources of Phanerozoic granitoids in central Asia: Sm-Nd isotope data[J]. Geochemistry, (8): 699~712(in Russiian).
[77]  [25]Kovalenko V I, Yarmolyuk V V, Thareva G M, et al. 1997. Sources of granitic magma in southern Dthir mineralized area, southeastern Mongolia: data of Nd, Sr, Pb and O isotope composition[J]. Rep. Acad. Sci., 353: 659~662(in Russian).
[78]  [26]Kovalenko V I, Kastitsin Y A, Yarmolyuk V V, et al. 1999. Magma sources and isotope (Sr, Nd) evolution of the rare-metal Li-F granites[J]. Petrology, 7(4): 401~429(in Chinese).
[79]  [27]Kozlov V D, Sandimirova G P, Pakholchenko YA, et al. 1995. On Mesozoic age of ore-bearing granites of the Kyzyl-Tau massif (Mongolian Altai)[J]. Geology and Geophysics, 36(3): 73~77(in Russian).
[80]  [28]Li H Q, Xie C F, Chang H L, et al. 1998. Study on metallogenetic chronology of nonferrous and precious metallic ore deposits in north Xinjiang, China[M]. Beijing: Geol. Pub. House. 263p(in Chinese with English abstract).
[81]  [29]McCulloch M T and Chappell B W. 1982. Nd isotopic characteristics of S- and I-type granites[J]. Earth Planet.Sci.Lett., 58: 51~64.
[82]  [30]Metal Mining Agency of Japan (MMAJ). 1998. Mineral Resources Map of Asia and list of metallic minerals deposits in Asia[M].
[83]  [31]Nie F J and Jiang S H. 2000. Discovery and its exploration significance of Talin Mettes Uul gold mineralized belt, south Mongolia[J]. Geology of Inner Mongolia, (2): 20~23(in Chinese with English abstract).
[84]  [32]Nie F J, Pei R F, Wu L S, et al. 1993. Magmatic activity and metallogeny of the Bainaimiao district, Inner Mongolia, China[M]. Beijing: Beijing Sci. & Technol.. Press. 239p(in Chinese with English abstract).
[85]  [33]Patchett P J. 1992. Isotopic studies of Proterozoic crustal growth and evolution[A]. In: Candie K C, ed. Proterozoic crustal evolution[C]. Amsterdam: Elsevier. 481~508.
[86]  [64]杜琦. 1988. 多宝山斑岩铜矿床[M]. 北京: 地质出版社. 386页.
[87]  [65]贺伯初, 谭克仁, 吴堑虹. 1994. 北疆吉木乃布氏金矿幔源岩浆岩时代及Sr、Nd同位素证据[J]. 大地构造与成矿学, 18(3): 219~228.
[88]  [66]洪大卫, 黄怀曾, 肖宜君, 等. 1994. 内蒙古中部二叠纪碱性花岗岩及其地球动力学意义[J]. 地质学报, 68(3): 217~230.
[89]  [67]洪大卫, 王式光, 谢锡林, 等. 2000. 兴蒙造山带正εNd(T)值花岗岩的成因和大陆地壳生长[J]. 地学前缘, 7(2): 441~456.
[90]  [68]姬金生, 陶洪祥, 杨兴科, 等. 1994. 东天山康古尔塔格金矿带地质与找矿[M]. 北京: 地质出版社. 200页.
[91]  [69]李华芹, 谢才富, 常海亮, 等. 1998. 新疆北部有色贵金属矿床成矿作用年代学[M]. 北京: 地质出版社. 263页.

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