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矿床地质  2013 

吉林汪清夹皮沟斑岩型钼矿床的形成时代与成矿构造背景

Keywords: 地球化学,锆石U-Pb年龄,辉钼矿Re-Os年龄,成矿构造背景,夹皮沟

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Abstract:

夹皮沟钼矿床是吉林省汪清县近年来发现的一个中型斑岩型钼矿床。矿体赋存在受北东向断裂控制的似斑状黑云母二长花岗岩内。含矿岩体中锆石LA-ICP-MSU-Pb加权平均年龄为(193.1±1.0)Ma(MSWD=1.02),矿石中辉钼矿Re-Os等时线年龄为(188.6±4.7)Ma(MSWD=0.41),表明夹皮沟钼矿床形成于早侏罗世,与区域内其他斑岩型钼矿床(成岩成矿时代介于190~160Ma)同属于燕山早期大规模构造-岩浆-成矿事件的产物。似斑状黑云母二长花岗岩具有高硅[w(SiO2)=72.29%~72.81%]、富碱[w(Na2O+K2O)=7.62%~7.71%]的特点,属于弱过铝质的高钾钙碱性岩石系列;稀土元素分布型式呈明显的右倾型,轻、重稀土元素分馏明显(LREE/HREE为6.41~7.34),Eu异常中等(δEu=0.33~0.40);微量元素组成上表现为富集大离子亲石元素(LILE),亏损高场强元素(HFSE)。似斑状黑云母二长花岗岩属于I型花岗岩,矿床成岩成矿物质可能源于俯冲背景下增厚的下地壳。结合区域地质构造演化,认为夹皮沟钼矿形成于古亚洲洋构造体制与环太平洋构造体制叠加与转换的构造背景下,成岩成矿作用与燕山早期古太平洋板块的俯冲作用关系密切。

References

[1]  葛文春,吴福元,周长勇,张吉衡. 2007. 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[J]. 科学通报,52(20):2407-2417.
[2]  黄 凡,陈毓川,王登红,袁忠信,陈郑辉. 2011. 中国钼矿主要矿集区及其资源潜力探讨[J]. 中国地质,38(5):1111-1134.
[3]  鞠 楠,任云生,王 超,王 辉,赵华雷,屈文俊. 2012. 吉林敦化大石河钼矿床成因与辉钼矿Re-Os同位素测年[J]. 世界地质,31(1):68-76.
[4]  李立兴,松权衡,王登红,王成辉,屈文俊,汪志刚,毕守业,于 城. 2009. 吉林福安堡钼矿中辉钼矿铼-锇同位素定年及成矿作用探讨[J]. 岩矿测试,28(3):283-287.
[5]  刘永江,张兴洲,金 巍,迟效国,王成文,马志红,韩国卿,温泉波,赵英利,王文弟,赵喜峰. 2010. 东北地区晚古生代区域构造演化[J]. 中国地质,37(4):943-951.
[6]  卢良兆,林 强,刘招君. 2004. 成因岩石学[M]. 长春:吉林大学出版社. 1-420.
[7]  罗铭玖,张辅民,董群英,许永仁,黎世美,李昆华. 1991. 中国钼矿床[M]. 郑州:河南科学技术出版社. 1-447.
[8]  苗来成,范蔚茗,张福勤,刘敦一,简 平,施光海,陶 华,石玉若. 2003. 小兴安岭西北部新开岭-科洛杂岩锆石SHRIMP年代学研究及其意义[J]. 科学通报,48(22):2315-2323.
[9]  邱家骧. 1991. 应用岩浆岩岩石学[M]. 武汉:中国地质大学出版社. 1-414.
[10]  孙德有. 2001. 张广才岭中生代花岗岩成因及其地球动力学意义(博士论文). 导师:林强,吴福元. 长春:吉林大学. 112页. 孙德有,吴福元,张艳斌,高 山. 2004a. 西拉木伦河-长春-延吉板块缝合带的最后闭合时间——来自吉林大玉山花岗岩体的证据[J]. 吉林大学学报(地球科学版),34(2):174-181.
[11]  孙德有,吴福元,高 山. 2004b. 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,25(2):213-218.
[12]  孙德有,吴福元,高 山,路孝平. 2005. 吉林中部晚三叠世和早侏罗世两期铝质A型花岗岩的厘定及对吉黑东部构造格局的制约[J]. 地学前缘,12(2):263-275.
[13]  孙景贵,张 勇,邢树文,赵克强,张增杰,白令安,马玉波,刘勇胜. 2012. 兴蒙造山带东缘内生钼矿床的成因类型、成矿年代及成矿动力学背景[J]. 岩石学报,28(4):1317-1332.
[14]  孙晓猛,刘永江,孙庆春,韩国卿,王书琴,王英德. 2008. 敦密断裂带走滑运动的40Ar/39Ar年代学证据[J]. 吉林大学学报(地球科学版),38(6):965-972.
[15]  孙珍军. 2010. 小兴安岭石林公园钼-钨-成矿作用及地球化学特征(硕士论文). 导师:孙国胜. 长春:吉林大学. 66页. 隋振民,葛文春,吴福元,张吉衡,徐学纯,程瑞玉. 2007. 大兴安岭东北部侏罗纪花岗质岩石的锆石U-Pb年龄、地球化学特征及成因[J]. 岩石学报,23(2):461-480.
[16]  王成辉,松权衡,王登红,李立兴,于 城,汪志刚,屈文俊,杜安道,应立娟. 2009. 吉林大黑山超大型钼矿辉钼矿铼-锇同位素定年及其地质意义[J]. 岩矿测试,28(3):269-273.
[17]  王成文,金 巍,张兴洲,马志红,迟效国,刘永江,李 宁. 2008. 东北及邻区晚古生代大地构造属性新认识[J]. 地层学杂志,32(2):119-136.
[18]  更多...
[19]  王 辉,任云生,赵华雷,鞠 楠,屈文俊. 2011. 吉林安图刘生店钼矿床辉钼矿Re-Os同位素定年及其地质意义[J]. 地球学报,32(6):707-715.
[20]  杨言辰,韩世炯,孙德有,郭 嘉,张苏江. 2012. 小兴安岭-张广才岭成矿带斑岩型钼矿床岩石地球化学特征及其年代学研究[J]. 岩石学报,28(2):379-390.
[21]  曾庆栋,刘建明,褚少雄,付国立,于文斌,李泽明,高玉友,李元九,孙 燕,周伶俐,段晓侠,张 松,王永彬. 2011. 西拉沐伦成矿带中生代花岗岩浆活动与钼成矿作用. 吉林大学学报(地球科学版),41(6):1705-1725.
[22]  曾 涛,王 涛,郭 磊,童 英,张建军,史兴俊,张 磊,李永飞. 2011. 东北新开岭地区晚中生代花岗岩类时代、成因及地质意义[J]. 吉林大学学报(地球科学版),41(6):1881-1900.
[23]  张 旗,李承东,王 焰,王元龙,金惟俊,贾秀勤,韩 松. 2005. 中国东部中生代高Sr低Yb和低Sr高Yb型花岗岩:对比及其地质意义[J]. 岩石学报,21(6):1527-1537.
[24]  张 旗,王 焰,李承东,王元龙,金惟俊,贾秀勤. 2006. 花岗岩的Sr-Yb分类及其地质意义[J]. 岩石学报,22(9):2249-2269.
[25]  张艳斌,吴福元,李惠民,路孝平,孙德友,周红英. 2002. 吉林黄泥河岭花岗岩体的单颗粒锆石U-Pb年龄[J]. 岩石学报,18(4):475-481.
[26]  张忠光,朴英姬,姜福平. 2011. 吉林省汪清县夹皮沟钼矿床特征及成因[J]. 吉林地质,30(4):29-43. 翟裕生,吕古贤. 2002. 构造动力体制转换与成矿作用[J]. 地球学报,23(2):97-102.
[27]  周建波,张兴洲,马志红,刘 立,金 魏,张梅生,王成文,迟效国. 2009. 中国东北地区的构造格局与盆地演化[J]. 石油与天然气地质,30(5):530-538.
[28]  Andersen T. 2002. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 192: 59-79.
[29]  Chappell B W and White A J R. 1974. Two contrasting granite type[J]. Pacific Geology, 8: 173-174.
[30]  Eiler J M, Grawford A J, Elliott T R, Farley K A, Valley J W and Stolper E. 2000. Oxygen isotope geochemistry of oceanic arc lavas[J]. Journal of Petrology, 41: 229-256.
[31]  Gill J B. 1981. Orogenic andesites and Plate tectonics[M]. New York: Springer Verlag. 1-385.
[32]  Grove T L and Donnelly N M. 1986. The evolution of young sillic lavas at Medicine Lake Volcano, California: Implications for the origin of compositional gaps in calcalkaline series lavas[J]. Contributions to Mineralogy and Petrology, 92: 281-302.
[33]  Liu Y S, Hu Z C, Gao S, Günther D, Xu J, Gao C G and Chen H H. 2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 257: 34-43.
[34]  Liu Y S, Gao S, Hu Z C, Gao C G, Zong K Q and Wang D. 2010. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths[J]. Journal of Petrology, 51: 537-571.
[35]  Ludwig K R. 2003. User\'s manual for isoplot 3.1, A geochronological toolkit for Microsoft Excle[M]. Berkeley: Geochronology Center Special Publication.4: 25-32.
[36]  Mao J W, Zhang Z C, Zhang Z H and Du A D. 1999. Re-Os isotopic dating of molybdenites in the Xiaoliugou W(Mo) deposit in the northern Qilian mountains and its geological significance[J]. Geochim. Cosmochim. Acta, 63(11-12): 1815-1818.
[37]  Mao J W, Pirajno F, Xiang J F, Gao J J, Ye H S, Li Y F and Guo B J. 2011. Mesozoic molybdenum deposits in the east Qinling-Dabie orogenic belt: Characteristics and tectonic settings[J]. Ore Geology Reviews, 43: 464-293.
[38]  Pearce J A, Harris N B W and Tindle A G, 1984. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 25: 956-983.
[39]  Peccerillo R and Taylor S R. 1976. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey[J]. Contributions to Mineralogy and Petrology, 58(1): 63-81.
[40]  Qi L, Hu J D and Conrad G. 2000. Determination of trace elements in granites by inductively coupled plasma mass spectrometry[J]. Talanta, 51: 507-513.
[41]  Rickwood P C. 1989. Boundary lines within petrologic diagram which use oxides of major and minor elements[J]. Lithos, 22(4): 247-263.
[42]  Smoliar M I, Walker R J and Morgan J W. 1996. Re-Os ages of Group IIA, IIIA, IVA, and IVB iron meteorites[J]. Science, 271: 1099-1102. Shirey S B and Walker R J. 1995. Carius tube digestion for low-blank rhenium-osmium analysis[J]. Analgtical Chemistry, 67: 2136-2141.
[43]  Sun S S and McDonough W F. 1989. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes. In: Saunders A D and Norry M J, eds. Magmatism in the Ocean Basins. London: Geological Society of Special Publication. 42: 313-345.
[44]  Wang F, Xu W L, Meng E, Cao H H and Gao F H. 2011. Early Paleozoic amalgamation of the Songnen-Zhangguangcai Range and Jiamusi massifs in the eastern segment of the Central Asian Orogenic Belt: Geochronological and geochemical evidence from granitoids and rhyolites[J]. Journal of Asian Earth Sciences 49, 234-248.
[45]  Whalen J B, Currie K L and Chappell B W. 1987. A-type granites: Geochemical characteristics, discrimination and petrogenesis[J]. Contrib. Mineral. Petrol., 95: 407-419.
[46]  Wu F Y, Sun D Y, Li H M, Jahn B M, Simon A and Wilde S A. 2002. A-type granites in northeastern China: Age and geochemical constraints on their petrogenesis. Chemical Geology, 187: 143-173.
[47]  Wu F Y, Jahn B M, Wilde S A, Lo C H, Yui T F, Lin Q, Ge W C and Sun D Y. 2003a. Highly fractionated I-type granites in NE China (I): Geochronology and petrogenesis[J]. Lithos, 66: 241-273.
[48]  Wu F Y, Jahn B M, Wilde S A, Lo C H, Yui T F, Lin Q, Ge W C and Sun D Y. 2003b. Highly fractionated I-type granites in NE China (II): isotopic geochemistry and implications for crustal growth in the Phanerozoic[J]. Lithos, 67: 191-204.
[49]  Wu F Y, Sun D Y, Jahn B M and Wilde S A. 2004. A Jurassic garnet-bearing granitic pluton from NE China showing tetrad REE patterns[J]. Journal of Asian Earth Sciences, 23: 731-744.
[50]  Wu F Y, Zhao G C, Sun D Y, Wilde S A and Yang J H. 2007. The Hulan Group: Its role in the evolution of the Central Asian Orogenic Belt of NE China[J]. Journal of Asian Earth Sciences, 30: 542-556.
[51]  Wu F Y, Sun D Y, Ge W C, Zhang Y B, Grant M L, Wilde S A and Jahn B M. 2011. Geochronology of the Phanerozoic granitoids in northeastern China[J]. Journal of Asian Earth Sciences, 41: 1-30.
[52]  Xiao W J, Windley B F, Hao J and Zhai M G. 2003. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt[J]. Tectonics, 22(6): 1-20.
[53]  Zhang Y B, Wu F Y, Zhai M G and Lu X P. 2004. The tectonic attributes of the Helong block and the eastern borderline of the north margin of North China[J]. Science in China (Series D), 34(9): 475-481.
[54]  陈 静. 2011. 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). 导师: 孙丰月. 长春: 吉林大学. 150页. 陈志广,张连昌,万 博,张玉涛,吴华英. 2008. 内蒙古乌奴格吐山斑岩铜钼矿床低Sr-Yb型成矿斑岩地球化学特征及地质意义[J]. 岩石学报,24(1):115-128.
[55]  代军治,毛景文,杨富全,叶会寿,赵财胜,谢桂青,张长青. 2006. 华北地台北缘燕辽钼(铜)成矿带矿床地质特征及动力学背景[J]. 矿床地质,25(5):598-612.
[56]  杜安道,屈文俊,李 超,杨 刚. 2009. 铼-锇同位素定年方法及分析测试技术的进展. 岩矿测试,28(3):288-304.

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