世界地质 2017, 36(2) 474-485 DOI:   10.3969/j.issn.1004-5589.2017.02.014  ISSN: 1004-5589 CN: 22-1111/P

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本文关键词相关文章
大兴安岭霍洛台
花岗闪长岩
锆石U-Pb年龄
岩石地球化学
构造环境
本文作者相关文章
PubMed
大兴安岭北段霍洛台铜铅锌矿区花岗闪长岩的岩石成因:地球化学和锆石U-Pb年代学制约
尚毅广1,2, 孙丰月1, 姜和芳1, 王启1, 尹悦1, 孟庆鹏1, 张志颖1
1. 吉林大学地球科学学院, 长春 130061;
2. 黑龙江省齐齐哈尔矿产勘查开发总院, 黑龙江齐齐哈尔 161000
摘要

黑龙江省大兴安岭地区霍洛台花岗闪长岩的锆石LA-ICP-MS U-Pb年代学表明,霍洛台花岗闪长岩(145 Ma)为早白垩世岩浆侵入产物。元素地球化学组成表明,为一套具埃达克岩特征的高钾钙碱性系列岩石,表现为高SiO2(65.64%~66.00%)、高K2O(3.67%~3.77%)、低MgO(0.09%~1.21%)、高Sr含量(814.00×10-6~893.00×10-6),低Yb(0.194×10-6~0.536×10-6)和Y(6.38×10-6~7.73×10-6),A/CNK为0.94~0.958,轻重稀土元素分异明显。La/Yb(92.54~245.88)、Th/La(0.17~0.2)、Th/U(4.01~4.84)和Mg#值(26.70~29.22)等特征显示霍洛台花岗闪长岩为加厚下地壳部分熔融形成。结合区域构造演化背景,认为霍洛台花岗闪长岩为受蒙古—鄂霍茨克构造体系影响下地壳加厚挤压-伸展转换阶段作用产物。

关键词 大兴安岭霍洛台   花岗闪长岩   锆石U-Pb年龄   岩石地球化学   构造环境  
Petrogenesis of granodiorites in Huoluotai Cu-Pb-Zn mining area: constrain from geochemistry and zircon U-Pb geochronology,northern Daxing'anling
SHANG Yi-guang1,2, SUN Feng-yue1, JIANG He-fang1, WANG Qi1, YIN Yue1, MENG Qing-peng1, ZHANG Zhi-ying1
1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. Heilongjiang Qiqihaer Mineral Exploration and Development Institute, Qiqihaer 161000, Heilongjiang, China
Abstract:

LA-ICP-MS U-Pb zircon geochronology of Huoluotai granodiorite of Daxing'anling area in Heillongjiang Province shows that Huoluotai granodiorite (145 Ma) results from magmatic intrusion of Early Cretaceous. The composition of elementary geochemistry indicates that it is a set of adakitic rocks characterized by high-K calc-alkaline series, with a high content of SiO2 (65.64%~66.00%) and K2O (3.67%~3.77%), low MgO (0.09%~1.21%), high content of Sr (814.00×10-6~893.00×10-6), low Yb (0.194×10-6 to 0.536×10-6) and Y (6.38×10-6 to 7.73×10-6), and obvious differentiation of light and heavy rare earth elements (10.1~14). The characteristics of La/Yb (92.54~245.88), Th/La (0.17~0.2), Th/U (4.01~4.84) and Mg# (26.70~29.22) show that the Huoluotai granodiorite was formed by partially melting of the thickened lower crust. Combined with regional tectonic evolution, it is concluded that the Huoluotai granodiorite originated from the transition process of crustal thickening compression to extension under the influence of Mongolia-Okhotsk tectonic system.

Keywords: Huoluotai of Daxinganling   granodiorite   zircon U-Pb chronology   geochemistry   tectonic environment  
收稿日期 2016-12-26 修回日期 2017-03-01 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2017.02.014
基金项目:

黑龙江省漠河县霍洛台铜、铅、锌矿普查项目(SDK2013-021).

通讯作者: 孙丰月(1963),男,教授,博士生导师,主要从事热液矿床成矿理论与预测、区域成矿作用研究.E-mail:sfy@jlu.edu.cn
作者简介:
作者Email: sfy@jlu.edu.cn

参考文献:

[1] Wu F Y,Sun D Y,Ge W C,et al. Geochronolgy of the Phanerozoic granitoids in northeastern China[J].Journal of Asian Earth Science,2011,41(1):1-30.
[2] 张兴洲,马玉霞,迟效国,等.东北及内蒙古东部地区显生宙构造演化的有关问题[J].吉林大学学报:地球科学版,2012,42(5):1269-1285. ZHANG Xing-zhou,MA Yu-xia,CHI Xiao-guo,et al.Discussion on Phanerozoic tectonic evolution in northeastern China[J].Journal of Jilin University:Earth Science Edition, 2012,42(5):1269-1285.
[3] 秦秀峰,尹志刚,汪岩,等.大兴安岭北端漠河地区早古生代埃达克质岩特征及地质意义[J].岩石学报.2007,23(6):1501-1511. QIN Xiu-feng,YIN Zhi-gang,WANG Yan,et al.Early Paleozoic adaktic rock in Mohe area at the northern end of the Da Hinggan Mountains and their geological significance[J].Acta Petrologica Sinica,2007,23(6):1501-1511.
[4] 宋彪,张玉海,万俞生,等.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论[J].地质论评,2002,48(增刊) : 26-30. SONG Biao,ZHANG Yu-hai,WAN Yu-sheng,et al.Mount making and procedure of the SHRIMP dating[J].Geological Review,2002,48(Suppl.):26-30.
[5] 袁洪林,吴福元,高山,等.东北地区新生代侵入体的锆石激光探针U-Pb年龄测定与稀土元素成分分析[J].科学通报,2003,48(14):1511-1520. YUAN Hong-lin,WU Fu-yuan,GAO Shan,et al.Determination of U-Pb age and trace element of zircon of Cenozoic intrusion in NE China by Laser-Ablation in ductively couple plasma mass spectrometry[J].China Science Bulletin,2003,48(14):1511-1520.
[6] YANG Hong-lin,GAO Shan,LIU Xiao-ming,et al.Accurate U-Pb age and trace element determinations of zircon by laser ablation-inductively coupled plasma-mass spectrometry[J].Geostandards and Geoanalytical Research,2004,28(3):353-370.
[7] Anderson T.Correction of common lead in U-Pb analyses that do not report 204Pb[J].Chemical Geology,2002,192(1/2):59-79.
[8] LIU Yong-sheng,HU Zhao-chu,GAO Shan,et al.In situ analysis of major and trace elements anhydrous minerals by LA-ICP-MS without applying an internal standards[J].Chemical Geology,2008,257(1/2):34-43.
[9] LIU Yong-sheng,GAO Shan,HU Zhao-chu,et al.Continental and oceanic crust recycling-induced melt-periotite interactions in the Trans-North China orogen:U-Pb dating,Hf isotopes and trace elements in zircons from mantle xenoliths [J].Journal of Petrology,2010,51(1/2):537-571.
[10] Ludwig K R.User's manual for isoplot 3.00: a geochronological toolkit for Microsoft Execl [J].Berkeley Geochronology Center Special Publication,2003,4:1-70.
[11] Irvine T N,Baragar W R A.A guide to the chemical classification of the common volcanic rocks [J].Canadian Journal of Earth Sciences,1971,8(5): 523-548.
[12] Sun S S,Mcdonough W F.Chemical and isotopic systematics of oceanic basalts:implication for mantle composition and processes[C]//Saunders A D,Norry M J.Magmatism in the ocean basins.Geological Society Special Publication,1989,42: 313-345.
[13] Macpherson C G,Dreher S T,Thirlwall M F.Adakites without slab melting: high pressure differentiation of island arc magma,Mindanao,the Philippines[J].Earth and Planetary Science Letters, 2006,243(3/4):581-593.
[14] 章凤奇,陈汉林,曹瑞成,等.海拉尔盆地基底晚古生代adakite的发现及其地质意义[J].岩石学报,2010,26(2):633-641. ZHANG Feng-qi,CHEN Han-lin,CAO Rui-cheng,et al.Discovery of Late Paleozoic adakite from the basement of the Hailaer Basin in NE China and its geological implication[J].Acta Petrologica Sinica,2010,26(2):633-641.
[15] Xu J F,Shinjo R,Defant M J,et al.Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of East China:partial melting of delaminated lower continental crust?[J].Geology,2002,30(12):1111-1114.
[16] Wang Q,Wyman D A,Xu J F,et al.Petrogenesis of Cretaceous adakitic and shoshonitic igneous rocks in the Luzong area,Anhui Province (eastern China):implications for geodynamics and Cu-Au mineralization[J].Lithos,2006,89(3/4):424-446.
[17] Wang Q,Wyman D A,Xu J F,et al.Partial melting of thickened or delaminated lower crust in the middle of eastern China:implications for Cu-Au mineralization[J].Journal of Geology,2007,115(2):149-161.
[18] 张旗,王焰,钱青,等.中国东部燕山期埃达克岩的特征及其构造-成矿意义[J].岩石学报,2001,17(2):236-244. ZHANG Qi,WANG Yan,QIAN Qing,et al.The characteristics and tectonic-metallogenic significances of the adakites in Yanshan period from eastern China[J].Acta Petrologica Sinica,2001,17(2):236-244.
[19] 许文良,王枫,孟恩,等.黑龙江省东部古生代—早中生代的构造演化:火成岩组合与碎屑锆石U-Pb年代学证据[J].吉林大学学报:地球科学版,2012,42(5) :1378-1389. XU Wen-liang,WANG Feng,MENG En,et al.Paleozoic-Early Mesozoic tectonic evolution in the eastern Heilongjiang Province,NE China:evidence from igneous rock association and U-Pb geochronology of detrital zircons[J].Journal of Jilin University:Earth Science Edition,2012,42(5) :1378-1389.
[20] Smithies R H.The Archaean tonalite-trondhjemite-granodiorite (TTG) series is not an analogue of Cenozoic adakite[J].Earth and Planetary Science Letters, 2000,182(1):115-125.
[21] Defant M J,Drummond M S. Derivation of some modern arc magmas by melting of young subducted lithosphere[J].Nature,1990, 374: 662-665.
[22] 卢良兆,许文良.岩石学[M].北京:地质出版社,2011:1-377. LU Liang-zhao,XU Wen-liang.Petrology[M].Beijing:Geological Publishing House,2011:1-377.
[23] 葛文春,吴福元,周长勇,等.大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约[J].科学通报,2005,50(12):1239-1247. GE Wen-chun,WU Fu-yuan,ZHOU Chang-yong,et al.The age of the Tahe granite pluton in northern Greater Khingan Range and its constraints on the tectonic attribution of the Eergu'na block[J].Chinese Science Bulletin,2005,50(12):1239-1247.
[24] XU Wen-liang, JI Wei-qiang, PEI Fu-ping, et al.Triassic volcanism in eastern Heilongjiang and Jilin provinces,NE China:chronology,geochemistry,and tectonic implications [J].Journal of Asian Earth Sciences,2009,34(3):392-402.
[25] 许文良,王枫,裴福萍,等.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约[J].岩石学报,2013,29(2):339-353. XU Wen-liang,WANG Feng,PEI Fu-ping,et al.Mesozoic tectonic regimes an regional ore-forming background in NE China:constraints from spatial and temporal variations of Mesozoic volcanic rock associations[J].Acta Petrologica Sinica,2013,29(2):339-353.
[26] 张宏,权恒,张炯飞,等.额尔古纳地区中生代火山岩形成的动力学环境[J].火山地质与矿产,1999,20(1):35-47. ZHANG Hong,QUAN Heng,ZHANG Jiong-fei,et al.Dynamic background of Mesozoic volcanic activity in Eergu'na region[J].Volcanology & Mineral Resources,1999,20(1):35-47.
[27] 王伟.满洲里—额尔古纳地区早侏罗世火山岩的年代学与地球化学研究:硕士学位论文[D].长春:吉林大学,2014. WANG Wei.Geochronology and geochemistry of the Early Jurassic volcanic rocks in the Manzhouli-Erguna area,NE China: master's degree thesis[D].Changchun: Jilin University,2014.
[28] Sun D Y,Gou J,Wang T H,et al.Geochronological and geochemical constraints on the Erguna Massif basement,NE China-subduction history of the Mongol-Okhotsk oceanic crust[J].International Geology Review,2013,55(14):1801-1816.
[29] 唐杰.额尔古纳地块中生代火成岩的年代学与地球化学:对蒙古—鄂霍茨克缝合带构造演化的制约:博士学位论文[D].长春:吉林大学,2016. TANG Jie.Geochronology and geochemistry of the Mesozoic igneous rocks in the Erguna Massif,NE China:constraints on the tectonic evolution of the Mongol-Okhotsk suture zone:doctor's degree thesis [D].Changchun: Jilin University,2016.
[30] 程瑞玉,吴福元,葛文春,等.黑龙江省东部饶河杂岩的就位时代与东北东部中生代构造演化[J].岩石学报,2006,22(2):353-376. CHENG Rui-yu,WU Fu-yuan,GE Wen-chun,et al.Emplacemet age of the Raohe complex in eastern Heilongjiang Province and the tectonic evolution of the eastern part of northeastern China[J].Acta Petrologica Sinica,2006,22(2):353-376.
[31] 王天豪,张书义,孙德有,等.满洲里南部中生代花岗岩的锆石U-Pb年龄及Hf同位素特征[J].世界地质,2014,33(1):26-38. WANG Tian-hao,ZHANG Shu-yi,SUN De-you,et al.Zircon U-Pb ages and Hf isotopic characteristics of Mesozoic granitoids from southern Manzhouli,Inner Mongolia[J].Global Geology,2014,33(1):26-38.
[32] 佘宏全,李进文,向安平,等.大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系[J].岩石学报,2012,28(2):571-594. SHE Hong-quan,LI Jin-wen,XIANG An-ping,et al.U-Pb ages of the zircons from primary rocks in middle-northern Daxinganling and its implications to geotectonic evolution[J].Acta Petrologica Sinica,2012,28(2):571-594.
[33] 张彦龙,葛文春,柳小明,等.大兴安岭新林镇岩体的同位素特征及其地质意义[J].吉林大学学报:地球科学版,2008,38(2):177-186. ZHANG Yan-long,GE Wen-chun,LIU Xiao-ming,et al.Isotopic characteristics and its significance of the Xinlin Town Pluton,Great Hinggan Mountains[J].Journal of Jilin University:Earth Science Edition,2008,38(2):177-186.
[34] 许文良,裴福萍,高福红,等.伊舒地堑基底花岗岩的锆石U-Pb年代学及其构造意义[J].地球科学,2008,33(2):145-150. XU Wen-liang,PEI Fu-ping,GAO Fu-hong,et al.Zircon U-Pb age from basement granites in Yishu graben and its tectonic implications[J]. Earth Science Edition,2008,33(2):145-150.
[35] 王伟,许文良,王枫,等.满洲里—额尔古纳地区中生代花岗岩的锆石U-Pb年代学与岩石组合:对区域构造演化的制约[J].高校地质学报,2012,18(1):88-105. WANG Wei,XU Wen-liang,WANG Feng,et al.Zircon U-Pb Chronology and assemblages of Mesozoic granitoids in the Manzhouli-Erguna area,NE China: constraints on the regional tectonic evolution[J].Geological Journal of China Universities,2012,18(1):88-105.
[36] 李宇,丁磊磊,许文良,等.孙吴地区中侏罗世白云母花岗岩的年代学与地球化学:对蒙古-鄂霍茨克洋闭合时间的限定[J].岩石学报,2015,31(1):56-66. LI Yu,DING Lei-lei,XU Wen-liang,et al.Geochronology and geochemistry of muscovite granite in Sunwu area,NE China: implications for the timing of closure of the Mongol-Okhotsk Ocean[J].Acta Petrologica Sinica,2015,31(1):56-66.

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