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矿床地质  2005 

东秦岭钼矿类型、特征、成矿时代及其地球动力学背景

Keywords: 地质学,东秦岭钼矿,时空分布,地球动力学背景,综述

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Abstract:

文章在总结前人研究成果的基础上,综合论述了东秦岭钼矿床的时空分布、分类和基本特征。东秦岭钼矿带沿区域构造线呈近东西向狭长带状展布,钼矿床主要集中分布于金堆城—南泥湖地区内;其形成与燕山期中酸性浅成_超浅成小花岗斑岩体有关,钼矿床直接产于岩体内外接触带及其附近;矿床类型主要为斑岩型、斑岩_矽卡岩型,少量热液碳酸盐脉型。结合Re_Os同位素年龄数据,探讨了东秦岭钼矿床的成矿时代及其成矿物质来源、成矿环境、大规模成矿作用时限及其特征,以及成矿地球动力学背景、演化特点和成矿过程。研究结果表明:除黄龙铺钼矿床形成于(221.5±0.3)Ma外,东秦岭地区钼矿床的大规模成矿主要出现在(144.8±2.1)~(132.4±2.0)Ma时限之间,对应的地球动力学背景为华北克拉通与扬子克拉通的碰撞造山后陆内造山局部伸展过程、中国东部地球动力学体制大转换晚期岩石圈拆沉及伸展时期。

References

[1]  Ames L, Tilton G R and Zhou G.1993.Timing of collision of the Sino-Korean and Yangtze cratons:U-Pb zircon dating of coesite-bearing eclogites[J]. Geology, 21:339~343.
[2]  Cheng Y J, Li C, Zhang J, et al.2000.Sr and O characteristics of porphyries in Qinling molybdemum deposit belt and their implication to genetic mechanism and type[J]. Science in China(Series D), 30(Supp.):65~72(in Chinese)..
[3]  Chu X C, Wang H Z, Shen X G, et al. 1992. Geology and mineral resource of Henan Province[M]. Beijing:Zhanwang Press of China. 632~638, 764~785(in Chinese).
[4]  Fan H R and Xie Y H.1999.Porphyry-type molybdenum deposits in the eastern Qinling Mo belt, central China[J]. Scientia Geologica Sinica, 8(1):91~101.
[5]  Farmer G L and Depaolo D J, 1987. Nd and Sr isotope study of hydrothemally altered granites at San Manud, Arizona:Implications for element migration paths during formation of porphy copper ore deposits[J]. Econ. Geol., 82:1142~1151.
[6]  Gao S, Zhang B R and Jin Z M.1999.The lower crustal delamination in Qinling-Dabie orogeny[J]. Science in China(Series D), 29(6):532~541(in Chinese).
[7]  Hu S X, Lin Q L, Chen Z M, et al. 1988. The geology and metallogeny of the amalgamation zone between ancient North China plate and South China plate (taking Qinling-Tongbai as an example)[M]. Nanjing:Press of Nanjing University. 442~489(in Chinese).
[8]  Hu Z H, Zhou S Z, Hu S X, et al. 1986. Characteristics of migmatites in Taihua Group of western Henan in relation to gold and molybdenum mineralizations[J]. Mineral Deposits, 5(4):71~81 (in Chinese with English abstract).
[9]  Hu Z H, Hu S X and Zhou S Z. 1990. The Yanshanian A-type twin granite belts of intracontinental compression-subduction environment in northern part of East Qinling area[J]. Acta Petrologica Sinica, (1):1~12(in Chinese with English abstract).
[10]  Huang D H, Wang Y C, Nie F J, et al. 1984a. Isotopic composition of sulfur, carbon and oxygen and source material of the Huanglongpu carbonatite vein-type of molybdenum(lead) deposits[J]. Acta Geologica Sinica, 58(3):252~264 (in Chinese with English abstract).
[11]  Huang D H, Nie F J, Wang Y C, et al. 1984b. Lead isotope compositions of molybdenum deposits in East Qinling as applied to the problem of ore sources[J]. Mineral Deposits, 3(4):20~28(in Chinese with English abstract).
[12]  Huang D H, Wang Y C, Nie F J, et al. 1985. A new type of molybdenum deposit-geological characteristics and metal-logenic mechanism of the Huanglongpu carbonatite vein-type of molybdenum(lead) deposit, Shaanxi[J]. Acta Geologica Sinica, 59(3):241~257(in Chinese with English abstract).
[13]  Huang D H, Wu C Y and Nie F J. 1987. Geological features and origin of the Jinduicheng porphyry molybdenum deposit, Shaanxi province[J]. Mineral Deposits, 6(3):22~34 (in Chinese with English abstract).
[14]  Huang D H, Dong Q Y, Gan Z X. 1989. Molybdenum deposits in China[A]. In:Song S H, ed. Chinese deposits[M]. Beijing:Geol. Pub. House. 482~512(in Chinese).
[15]  Huang D H, Wu C Y, Du A D, et al. 1994. Re-Os isotope age of molybdenum deposits in East Qinling and their significance[J]. Mineral Deposits, 13(3):221~230 (in Chinese with English abstract).
[16]  Huang D H, Du A D, Wu C Y, et al. 1996. Metallochronology of Mo(-Cu) deposits in the North China plateform:Re-Os age of molybdenite and its geological significance[J]. Mineral Deposits, 15(4):365~373 (in Chinese with English abstract).
[17]  Kroner A, Compston W, Zhang G W, et al. 1988. Age and tectonic setting of late Archean greenstone-gneiss terrain in Henan Province, China, as revealed by single-grain zircon dating[J]. Geology, 16:211~215.
[18]  Li J Y.2001.The collision time and way of Yangzte block and Sino-Korea block:Evolution of sediment environment at Yangtze Mid- Lower Valley during Sinian-Jurassic[J]. Acta Geologica Sinica, 75(1):25~34(in Chinese with English abstract).
[19]  Li S G, Hart S R, Zheng S G, et al. 1989. The collision time of North China plate and South China plate:Evidence from Sm-Nd ages[J]. Science in China(Series B), 19(3):312~319(in Chinese).
[20]  Li X Z, Yan Z and Lu X X.1993.Granites of Mt. Qinling and Dabie[M]. Beijing:Geol. Pub. House (in Chinese).
[21]  更多...
[22]  Li Y F, Mao J W, Bai F J, et al.2003.Re-Os isotopic dating of molybdenites in the Nannihu Mo(W) orefield in the eastern Qinling and its geological significace[J]. Geological Review, 49(6):652~659(in Chinese with English abstract).
[23]  Li Y F, Mao J W, Bai F J, et al. 2004a. Re-Os isotopic system and its application in geology[J]. Geology and Prospecting, 40(1):64~67(in Chinese with English abstract).
[24]  Li Y F, Mao J W, Guo B J, et al. 2004b. Re-Os isotopic dating of molybdenites in the Nannihu Mo(W) orefield in the eastern Qinling and its geodynamic process[J]. Acta Geologica Sinica(English Edition), 78(2):463~470.
[25]  Li Y F, Mao J W, Liu D Y, et al. 2005. SHRIMP zircon U-Pb and molybdenite Re-Os datings for the Leimengou porphyry Mo deposit, in western Henan Province, China and its geological implication[J]. Acta Geologica Sinica, (in press).
[26]  Liu X S, Yan Z F, Zheng S J, et al. 1987. Geological-geochemical studies on ore-hosting strata of the typical ore deposits in the Eastern Qinling nonferrous metallogenic belt[J]. Mineral Deposits, 6(4):1~10(in Chinese with English abstract).
[27]  Lu X X. 1994. Two types granites and two gold deposit series[J]. Geological Review, 40(5):418~428(in Chinese with English abstract).
[28]  Lu X X, Dong Y, Chang Q L, et al. 1996. Indosinian Shahewan rapakivi granite in Qinling and its dynamic significance[J]. Science in China(Series D), 39(3):266~272.
[29]  Lu X X, Yu Z P, Feng Y L, et al. 2002. Mineralization and tectonic setting of the deep-hypabyssal granites in East Qinling mountain[J]. Mineral Deposits, 21(2):168~178 (in Chinese with English abstract).
[30]  Luo M J, Zhang F M, Dong Q Y, et al. 1991. Molybdenum deposits in China[M]. Zhengzhou:Henan Press of Science and Technology. 118~128,403~408(in Chinese).
[31]  Luo M J, Li S M, Lu X X, et al.2000.The mineralization and minerogenetic series of major resource in Henan Province[M]. Beijing:Geol. Pub. House. 81~111(in Chinese).
[32]  Mao J W, Hua R M and Li X B. 1999a. A preliminary study of large-scale metallogenesis and large clusters of mineral deposits[J]. Mineral Deposits, 18(4):291~299 (in Chinese with English abstract).
[33]  Mao J W, Zhang Z C, Zhang Z H. et al. 1999b. Re-Os isotopic dating of molybdenites in the Xiaoliugou W(Mo) deposit in the northern Qilian mountains and its geological significance[J]. Geochimica et Cosmochimica Acta, 63(11-12):1815~1818.
[34]  Mao J W, Richard J G, Zhang Z W, et al. 2002. Gold deposits in the Xiaoqinling-Xiong\\'ershan region, Qinling mountains, central China[J]. Mineralium Deposita, 37:306~325.
[35]  Mao J W, Zhang Z H, Yu J J, et al.2003.The geodynamics setting of Mesozoic large-scale mineralization in North China:The revelation from accurate timing of metal deposits[J]. Science in China(Series D):33(4):289~299(in Chinese).
[36]  Mao J W, Xie G Q, Zhang Z H, et al. 2005. Mesozoic large-scale metallogenic pulses in North China and corresponding geodynamic setting[J]. Acta Petrologica Sinica, 21(1):169~188(in Chinese with English abstract).
[37]  Meng Q R and Zhang G W.1999.Timing of collision of the North and South China blocks:Controvery and reconciliation[J]. Geology, 2:123~126.
[38]  Niu B G, He Z J, Song B, et al.2003.The SHRIMP dataing of Zhangjiakou Formation volcanic rock and its important implications[J]. Geological Bulletin of China, 22(2):140~141(in Chinese).
[39]  Pei R F and Xiong Q Y.1999.Metallogenic provincetiality and metallotect convergence of unique ore deposits in China[J]. Mineral Deposits,18(1):37~46(in Chinese with English abstract).
[40]  Ren J S. 1991. A discussion on the basic features of the lithosphere tectonics in Chinese continents[J]. Regional Geology of China, 2:289~293 (in Chinese with English abstract).
[41]  Ren Q J, Wu Y B, Wu Y C, et al. 1987. Distribution pattern and origin of ore-bearing fissures in the Jinduicheng porphyry molybdenum deposit, Shaanxi Province[J]. Mineral Deposits, 6(3):35~48 (in Chinese with English abstract).
[42]  Stein H J, Markey R J, W Morgan J, et al.1997.Highly precise and accurate Re-Os ages for molybdenite from the East Qinling molybdenum belt, Shaanxi Province, China[J]. Econ. Geol., 92:827~835.
[43]  Stein H J, Markey R J, W Morgan J, et al.2001.The remarkable Re-Os chronometer in molybdenite:How and why it works[J]. Terra Nova, 13(6):479~486.
[44]  Taylor H P. 1977. Oxygen and hydrogen isotope relationships in hydrothermal mineral deposits[A]. In:Barnes H L, ed. Geochemistry of hydrothermal ore deposits[M]. Second Edition. John Wiley and Sons. 244~248.
[45]  Wang T C. 1985. Geological features of Leimengou molybdenum deposit[J].Henan Geology, 3(Supp.):270~272(in Chinese).
[46]  Xiao Q H, Deng J J, Ma D Q, et al. 2002. The ways of investigation on granitoids[M]. Beijing:Geol.Pub. House (in Chinese).
[47]  Xu Z W, Qiu J S, Ren Q J, et al. 1995. Characteristics of Yanshanian granites related to molybdenum-tungsten deposits in the southern part of Luanchuan County, Henan Province[J]. Acta Petrologica Sinica, 11(4):397~408(in Chinese with English abstract).
[48]  Xu Z W, Yang R Y, Liu H Y, et al.1998.Study on the ore-forming fluid of the Jinduicheng porphyry molybdenum deposit, Shaanxi Province[J]. Geological Journal of China University, 4(4):423~431(in Chinese with English abstract).
[49]  Xu Z Q, Lu Y L, Tang Y Q, et al. 1986. Deformation characteristics and tectonic evolution of the eastern Qinling orogenic belt[J]. Acta Geologica Sinica, 60(3):237~247(in Chinese with English abstract).
[50]  Zhang B R, Luo T C, Gao S, et al. 1994. Geochemical study of the lithosphere, tectonism and metallogenesis in the Qinling-Dabashan region[M]. Wuhan:Press of China University of Geoscience. 257~277(in Chinese).
[51]  Zhang B R, Zhang H F, Zhao Z D, et al. 1996. Geochemical subdivision and evolution of the lithosphere in East Qinling and adjacent regions:Implications for tectonics[J]. Science in China (Series D), 26(3):201~208 (in Chinese).
[52]  Zhang G W, Meng Q R, Yu Z P, et al. 1996. Orogenesis and dynamics of Qinling orogen[J]. Science in China (Series D), 26(3):193~200 (in Chinese).
[53]  Zhang G W, Meng Q R, Liu S F, et al.1997.Huge intracontinental subduction zone at south margin of North China block and present 3-D lithospheric framework of the Qinling orogenic belt[J]. Geological Journal of China University,3(2):129~143 (in Chinese with English abstract).
[54]  Zhang G W, Zhang B R, Yuan X C, et al.2001.Qinling orogenic belt and continental dynamics[M]. Beijing:Science Press.
[55]  Zhang Z W and Lu X X. 1989. Petrochemical characteristics of the granitoids in East Qinling[J]. Henan Geology, 7(3):44~54 (in Chinese with English abstract).
[56]  Zhang Z W and Deng J. 2001a. Geological setting of the eastern Qinling molybdenum ore belt and the features of the Mo-associated intrusions[A].In:Chen Y J, Zhang J and Lai Y, ed. Continental geodynamics and metallogenesis[C]. Beijing:Seismological Press. 100~109 (in Chinese).
[57]  Zhang Z W, Zhu B Q, Chang X Y, et al. 2001b. Petrogenetic metallogenetic background and time space relationship of the East Qinling molybdenum ore belt, China[J]. Geological Journal of China University, 7(3):307~315(in Chinese with English abstract).
[58]  Zhang Z W, Zhu B Q, Chang X Y, et al. 2001b. Petrogenetic metallogenetic background and time space relationship of the East Qinling molybdenum ore belt, China[J]. Geological Journal of China University, 7(3):307~315(in Chinese with English abstract).
[59]  Zhao T P, Zhou M F, Jin C W, et al.2001.Discussion on age of the Xiong\\'er Group in the southern margin of North China craton[J]. Chinese Journal of Geology, 36(3 ):326~334(in Chinese with English abstract).
[60]  Zhao Y, Yang Z Y and Ma X H. 1994. Geotectonic transition from paleoasian system and paleotethyan system to paleopacific active continental margin in Eastern Asia[J]. Scientia Geologica Sinica, 29(2):105~109 (in Chinese with English abstract).
[61]  Zhao Z H and Tu G C.2003.Superlarge-scale deposits in China(Ⅱ)[M]. Beijing:Science Press. 523~542.
[62]  李宪梓 严阵 卢欣祥.秦岭-大别山花岗岩[M].北京:地质出版社,1993..
[63]  李永峰 毛景文 白凤军 李俊平 和志军.东秦岭南泥湖钼(钨)矿田Re—Os同位素年龄及其地质意义[J].地质论评,2003,49(6):652-659,.
[64]  李永峰 毛景文 白凤军 王雨 李俊平.Re-Os同位素体系及其地质应用[J].地质与勘探,2004,40(1):64-67,.
[65]  李永峰 毛景文 刘敦一.豫西雷门沟斑岩钼矿SHRIMP锆石U—Pb及辉钼矿Re—Os测年及其地质意义[J].地质学报,2005:(待刊).
[66]  刘孝善 严正富 郑素娟.东秦岭有色金属成矿带中典型矿床赋矿地层的地质地球化学研究[J].矿床地质,1987,6(4):1-10.
[67]  卢欣祥.东秦岭两类花岗岩与两个金矿系列[J].地质论评,1994,40(5):418-428,.
[68]  卢欣祥 肖庆辉.秦岭印支期沙河湾奥长环斑花岗岩及其动力学意义[J].中国科学:D辑,1996,26(3):244-248,.
[69]  卢欣祥 于在平 等.东秦岭深源浅成型花岗岩的成矿作用及地质构造背景[J].矿床地质,2002,21(2):168-178,.
[70]  罗铭玖 张辅民 董群英.中国钼矿床[M].郑州:河南科学技术出版社,1991.452.
[71]  罗铭玖 黎世美 卢欣祥 等.河南省主要矿产的成矿作用及矿床成矿系列[M].北京:地质出版社,2000..
[72]  毛景文 华仁民.浅议大规模成矿作用与大型矿集区[J].矿床地质,1999,18(4):291-299,.
[73]  毛景文 张作衡 余金杰 王义天 牛宝贵.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[J].中国科学:D辑,2003,33(4):289-299,.
[74]  毛景文 谢桂青 张作衡 李晓峰 王义天 张长青 李永峰.中国北方中生代大规模成矿作用的期次及其地球动力学背景[J].岩石学报,2005,21(1):169-188,.
[75]  牛宝贵 和政军 等.张家口组火山岩SHRIMP定年及其重大意义[J].地质通报,2003,22(2):140-141,.
[76]  裴荣富 熊群尧.中国特大型金属矿床成矿偏在性与成矿构造聚敛(场)[J].矿床地质,1999,18(1):37-46,.
[77]  任纪舜.论中国大陆岩石圈构造的基本特征[J].中国区域地质,1991,(4):289-293,.
[78]  任启江 吴俞斌 武耀成.陕西金堆城斑岩钼矿含矿裂隙分布规律与成因[J].矿床地质,1987,6(3):35-48.
[79]  尚瑞钧 严阵.秦巴花岗岩[M].武汉:中国地质大学出版社,1988..
[80]  王天聪.雷门沟钼矿床地质特征[J].河南地质,1985,3(增刊):270-272.
[81]  肖庆辉 邓晋福 马大铨 等.花岗岩研究思维与方法[M].北京:地质出版社,2002..
[82]  徐兆文 杨荣勇.河南栾川南部地区与Mo—W矿床有关的燕山期花岗岩特征[J].岩石学报,1995,11(4):397-408,.
[83]  徐兆文 杨荣勇.陕西金堆城斑岩钼矿床成矿流体研究[J].高校地质学报,1998,4(4):423-431,.
[84]  许志琴.东秦岭造山带的变形特征及构造演化[J].地质学报,1986,60(3):237-247.
[85]  张本仁.秦巴岩石圈构造及成矿规律地球化学研究[M].武汉:中国地质出版社,1994..
[86]  张本仁 张宏飞 赵志丹.东秦岭及邻区壳、幔地球化学分区和演化及其大地构造意义[J].中国科学(D辑),1996,26(3):201-208.
[87]  张国伟 孟庆任.秦岭造山带的造山过程及其动力学特征[J].中国科学:D辑,1996,26(3):193-200,.
[88]  张国伟 孟庆任.华北地块南部巨型陆内俯冲带与秦岭造山带岩石圈现今三维结构[J].高校地质学报,1997,3(2):129-143,.
[89]  张国伟 张本仁 袁学诚 等.秦岭造山带与大陆动力学[M].北京:科学出版社,2001.432-449.
[90]  张正伟 卢欣祥 等.东秦岭花岗岩类岩石化学的统计特征[J].河南地质,1989,7(3):44-54,.
[91]  张正伟 邓军.东秦岭钼矿带成矿背景与含矿岩体特征[A].陈衍景 张静 赖勇 主编.大陆动力学与成矿作用[C].北京:地震出版社,2001a.100-109.
[92]  张正伟 朱炳泉 等.东秦岭钼矿带成岩成矿背景及时空统一性[J].高校地质学报,2001,7(3):307-315,.
[93]  张宗清 刘敦一 付国民.北秦岭变质地层秦岭、宽坪、陶湾群同位素年代研究[M].北京:地质出版社,1994.1-191.
[94]  赵太平 周美夫 等.华北陆块南缘熊耳群形成时代讨论[J].地质科学,2001,36(3):326-334,.
[95]  赵越.东亚大地构造发展的重要转折[J].地质科学,1994,29(2):105-119,.
[96]  赵振华 涂光炽.中国超大型矿床(Ⅱ)[M].北京:科学出版社,2003.54-56.
[97]  陈衍景 李超 等.秦岭钼矿带斑岩体锶氧同位素特征与岩石成因机制和类型[J].中国科学:D辑,2000,30(12):64-72,.
[98]  楚新春 王亨治 申学广.河南省地质矿产志[M].北京:中国展望出版社,1992.632-638,764-785.
[99]  高山 Kern.H.秦岭—大别造山带下地壳拆沉作用[J].中国科学:D辑,1999,29(6):532-541,.
[100]  胡受奚 林潜龙 陈泽铭.华北与华南古板块拼合带地质和成矿[M].南京:南京大学出版社,1988.442-489.
[101]  胡志宏 周顺之 胡受奚.豫西太华群混合岩特征及其与金钼矿化的关系[J].矿床地质,1986,5(4):71-81.
[102]  胡志宏 胡受奚.东秦岭燕山期大陆内部挤压—俯冲背景的A型孪生花岗岩带[J].岩石学报,1990,(1):1-12,.
[103]  黄典豪 王义昌 聂凤军.黄龙铺碳酸盐脉型钼(铅)矿矿床的硫、碳、氧同位素组成及成矿物质来源[J].地质学报,1984a,58(3):252~264.
[104]  黄典豪 聂凤军 王义昌.东秦岭地区钼矿床铅同位素组成特征及其成矿物质来源初探[J].矿床地质,19848,3(4):20~28.
[105]  黄典豪 王义昌 聂凤军.一种新的钼矿床类型——陕西黄龙铺碳酸盐脉型钼(铅)矿矿床地质特征及成矿机制[J].地质学报,1985,59(3):241-257.
[106]  黄典豪 吴澄宇 聂凤军.陕西金堆城斑岩钼矿床地质特征及成因探讨[J].矿床地质,1987,6(3):22-34.
[107]  黄典豪 董群英 甘志贤.中国钼矿床[A].宋叔和主编.中国矿床[C].北京:地质出版社,1989.482-512.
[108]  黄典豪 杜安道.东秦岭地区钼矿床的铼—锇同位素年龄及其意义[J].矿床地质,1994,13(3):221-230,.
[109]  黄典豪 杜安道.华北地台钼(铜)矿床成矿年代学研究:辉钼矿铼—锇年龄及其地质意义[J].矿床地质,1996,15(4):365-373,.
[110]  李锦轶.中朝地块与扬子地块碰撞的时限与方式——长江中下游地区震旦纪—侏罗纪沉积环境的演变[J].地质学报,2001,75(1):25-34.
[111]  李曙光 HartSR 郑双根.中国华北、华南陆块碰撞时代的Sm—Nd 同位素年龄证据[J].中国科学(B辑),1989,19(3):312~31.

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