世界地质    2019 38 (3): 655-667   ISSN: 1004-5589  CN: 22-1111/P   大兴安岭北段龙江地区早白垩世晶洞花岗岩的成因及构造意义 景妍1, 张彦龙1, 王清海2, 刘希雯3, 陈会军4 1. 吉林大学地球科学学院, 长春 130061; 2. 吉林大学东北亚国际地学研究与教学中心, 长春 130026; 3. 吉林省水利水电勘测设计研究院, 长春 130021; 4. 中国地质调查局 沈阳地质调查中心, 沈阳 110034 收稿日期 2019-04-10  修回日期 2019-06-03  网络版发布日期 null 参考文献  [1] Pearce J A, Harris N B W, Tindle A G. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 1984, 25(4):956-983. [2] Eby G N. Chemical subdivision of the A-type granitoids:petrogenetic and tectonic implications[J]. Geology, 1992, 20(7):641-644. [3] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1):1-30. [4] 内蒙古自治区地质矿产局.内蒙古自治区区域地质志[M].北京:地质出版社,1991:1-725. Inner Mongolia Bureau of Geology Mineral Resources. Regional geology of Inner Mongolia[M]. Beijing:Geological Publishing House, 1991:1-725. [5] Yu Q, Ge W C, Yang H, et al. Petrogenesis of Late Paleozoic volcanic rocks from the Daheshan Formation in central Jilin Province, NE China, and its tectonic implications:constraints from geochronology, geochemistry and S-Nd-Hf isotopes[J]. Lithos, 2014, 192:116-131. [6] 崔芳华,郑常青,徐学纯,等. 大兴安岭全胜林场地区晚石炭世岩浆活动研究:对兴安地块与松嫩地块拼合时间的限定[J].地质学报,2013,87(9):1247-1263. CUI Fang-hua, ZHENG Chang-qing, XU Xue-chun, et al. Late Carboniferous magmatic activities in the Quanshenglinchang area, Great Xing'an Range:constrains on the timing of amalgamation between Xing'an and Songnen massifs[J]. Acta Geologica Sinica, 2013, 87(9):1247-1263. [7] 李竞妍,郭锋,李超文,等.东北地区晚古生代-中生代I型和A型花岗岩Nd同位素变化趋势及其构造意义[J].岩石学报,2014,30(7):1995-2008. LI Jing-yan, GUO Feng, LI Chao-wen, et al. Neodymium isotopic variations of Late Paleozoic to Mesozoic I-and A-type granitoids in NE China:implications for tectonic evolution[J]. Acta Petrologica Sinica, 2014, 30(7):1995-2008. [8] 邵济安,张履桥,贾文,等.内蒙古喀喇沁变质核杂岩及其隆升机制探讨[J].岩石学报,2001,17(2):283-290. SHAO Ji-an, ZHANG Lü-qiao, JIA Wen, et al. Harkin metamorphic core complex in Inner Mongolia and its upwelling mechanism[J]. Acta Petrologica Sinica, 2001, 17(2):283-290. [9] Zhang J H, Ge W C, Wu F Y, et al. Large-scale Early Cretaceous volcanic events in the northern Great Xing'an Range,northeastern China[J]. Lithos, 2008, 102(1/2):138-157. [10] 葛文春,吴福元,周长勇,等.大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义[J].岩石学报,2005, 21(3):749-762. GE When-chun, WU Fu-yuan, ZHOU Chang-yong, et al. Zircon U-Pb ages and its significance of the Mesozoic granites in the Wulanhaote region, central Da Hinggan Mountaim[J]. Acta Petrologica Sinica, 2005, 21(3):749-762. [11] 葛文春,吴福元,周长勇,等.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,2007,52(20):2407-2417. GE When-chun, WU Fu-yuan, ZHOU Chang-yong, et al. Porphyry Cu-Mo deposits in the eastern Xing'an-Mongolian orogenic belt:mineralization ages and their geodynamic implications[J]. Chinese Science Bulletin, 2007, 52(20):2407-2417. [12] 张彦龙,赵旭晁,葛文春,等.大兴安岭北部塔河花岗杂岩体的地球化学特征及成因[J].岩石学报,2010,26(12):3507-3520. ZHANG Yan-long, ZHAO Xu-chao, GE Wen-chun, et al. Geochemical characteristics and genesis of Tahe granitic complex in northern part of the Da Hinggan Range[J]. Acta Petrologica Sinica, 2010, 26(12):3507-3520. [13] Wu F Y, Sun D Y, Li H M, et al. A-type granites in northeastern China:age and geochemical constraints on their petrogenesis[J]. Chemical Geology, 2002, 187(1/2):143-173. [14] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic granitoids in northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41(1):1-30. [15] Andersen T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002, 192(1/2):59-79. [16] 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 rare earth element concentrations of zircons from Cenozoic intrusions in northeastern China by laser ablation ICP-MS[J]. Science Bulletin, 2003, 48(14):1511-1520. [17] Wu F Y, Yang Y H, Xie L W, et al. Hf isotopic compositions of the standard zircons in U-Pb geochronology[J]. Chemical Geology, 2006, 234(1/2):105-126. [18] Koschek G. Origin and significance of the SEM cathodoluminescence from zircon[J]. Journal of Microscopy, 1993, 171(3):223-232. [19] Irvine T H, 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. [20] Peccerillo A, Taylor A R. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58(1):63-81. [21] Maniar P D, Piccoli P M. Tectonic discrimination of granitoids[J]. Geological Society of American Bulletin, 1989, 101(5):635-643. [22] Boynton W V. Geochemistry of the rare earth elements:meteorite studies[C]//Henderson P. Rare Earth Elements Geochemistry. Amsterdam:Elsevier, 1984:63-114. [23] Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and process[C]//Sauders A D, Norry M J. Magmatism in the Ocean Basins. Geological Society Special Publication, 1989:313-345. [24] Yang J H, Wu F Y, Shao J, et al. Constraints on the timing of uplift of the Yanshan fold and thrust belt, North China[J]. Earth and Planetary Science Letters, 2006, 246(3/4):336-352. [25] 田德欣,王清海,葛文春,等.内蒙古阿尔山绿水碱长花岗岩锆石U-Pb年龄、地球化学特征及构造意义[J].世界地质,2013,32(4):681-693. TIAN De-xin, WANG Qing-hai, GE Wen-chun, et al. Zircon U-Pb ages and geochemical characteristics of Lvshui alkali feldspar granites in Arshan, Inner Mongolia and their tectonic implications[J]. Global Geology, 2013, 32(4):681-693. [26] 施璐,郑常青,姚文贵,等.大兴安岭中段五岔沟地区蛤蟆沟林场A型花岗岩年代学、岩石地球化学及构造背景研究[J].地质学报,2013,87(9):1264-1276. SHI Lu, ZHENG Chang-qing, YAO Wen-gui, et al. Geochronology, petro-geochemistry and tectonic setting of the Hamagou forest farm A-type granites in the Wuchagou region, central Great Xinggan Range[J]. Acta Geologica Sinica, 2013, 87(9):1264-1276. [27] 陈会军,张彦龙,王清海,等.大兴安岭中段早白垩世花岗质岩石锆石U-Pb年龄及地球化学特征[J].地质与资源,2015,24(5):433-443. CHEN Hui-jun, ZHANG Yan-long, WANG Qing-hai, et al. Zircon U-Pb dating and geochemistry of the Early Cretaceous granitic rocks in the middle section of Daxinganling Mountains[J]. Geology and Resources, 2015, 24(5):433-443. [28] 和越,董玉,和钟铧,等.大兴安岭中北段早白垩世爱林源花岗岩的成因:锆石U-Pb年代学、地球化学及Hf同位素制约[J].世界地质,2017,36(3):701-713. HE Yue, DONG Yu, HE Zhong-hua, et al. Petrogenesis of Early Cretaceous Ailinyuan granites from northern-central Da Hinggan mountains:constraints from zircon U-Pb age, geochemistry and Hf isotopes[J]. Global Geology, 2017, 36(3):701-713. [29] Dong Y, Ge W C, Yang H, et al. Geochronology and geochemistry of Early Cretaceous volcanic rocks from the Baiyingaolao Formation in the central Great Xing'an Range, NE China, and its tectonic implications[J]. Lithos, 2014, 205:168-184. [30] Wang F, Xu W L, Meng E, et al. 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, 2012, 49:234-248. [31] Whalen J B, Currie K L, Chappell B W. A-type granites:geochemical characteristics, discrimination and petrogenesis[J]. Contributions to Mineralogy and Petrology, 1987, 95(4):407-419. [32] Chappell B W, White A J R. I-and S-type granites in the Lachlan fold belt[J]. Transactions of the Royal Society of Edinburgh:Earth and Environmental Science, 1992, 83(1/2):1-26. [33] Chappell B W. Aluminium saturation in I-and S-type granites and the characterization of fractionated haplogranites[J]. Lithos, 1999, 46(3):535-551. [34] Dong Y, Ge W C, Zhao G C, et al. Petrogenesis and tectonic setting of the Late Paleozoic Xing'an complex in the northern Great Xing'an Range, NE China:constraints from geochronology, geochemistry and zircon Hf isotopes[J]. Journal of Asian Earth Sciences, 2016, 115:228-246. [35] Ji Z, Ge W C, Wang Q H, et al. Petrogenesis of Early Cretaceous volcanic rocks of the Manketouebo Formation in the Wuchagou region, central Great Xing'an Range, NE China, and tectonic implications:geochronological, geochemical, and Hf isotopic evidence[J]. International Geology Review, 2016, 58(5):556-573. [36] Pearce J A, Harris N B W, Tindle A G, et al. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 1984, 25(4):956-983. [37] 李培忠,于津生.黑龙江碾子山晶洞碱性花岗岩岩体年龄及其意义[J].地球化学,1993,22(4):389-399. LI Pei-zhong, YU Jin-sheng. Nianzishan miarolitic alkaline granite stock, Heilongjiang:its ages and geological implications[J]. Geochimica, 1993, 22(4):389-399. [38] Jahn B M, Wu F Y, Capdevila R, et al. Highly evolved juvenile granites with tetrad REE patterns:the Woduhe and Baerzhe granites from the Great Xing'an Mountains in NE China[J]. Lithos, 2001, 59:171-198. [39] 杨钢,肖龙,高睿,等.内蒙古阿尔山地区中生代A型花岗岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其构造意义[J].地质通报,2014,33(5):649-660. YANG Gang, XIAO Long, GAO Rui, et al. Geochemistry and tectonic significance of Mesozoic A-type granites in Aershan area, Inner Mongolia[J]. Geological Bulletin of China, 2014, 33(5):649-660. [40] Wu F Y, Sun D Y, Li H, et al. A-type granites in northeastern China:age and geochemical constraints on their petrogenesis[J]. Chemical Geology, 2002, 187(1):143-173. [41] 王超,刘志宏,宋健,等.延边开山屯花岗闪长岩-石英闪长岩体年代学、地球化学特征及对古太平洋板块俯冲作用时限的制约[J].岩石学报,2016,32(9):2856-2866. WANG Chao, LIU Zhi-hong, SONG Jian, et al. Chronology, geochemical characteristics of granodiorite-quartz diorite pluton in Kaishantun, Yanbian area and its constrains to the beginning of Paleo-Pacific Plate subduction[J]. Acta Petrologica Sinica, 2016, 32(9):2856-2866. [42] Wang F, Zhou X H, Zhang L C, et al. Late Mesozoic volcanism in the Great Xing'an Range (NE China):timing and implications for the dynamic setting of NE-Asia[J]. Earth and Planetary Science Letters, 2006, 251(1/2):179-198. [43] 高晓峰,郭锋,范蔚茗,等.南兴安岭晚中生代中酸性火山岩的岩石成因[J].岩石学报,2005,21(3):737-748. GAO Xiao-feng, GUO Feng, FAN Wei-ming, et al. Origin of Late Mesozoic intermediate-felsic volcanic rocks from the northern Da Hinggan Mountain, NE China[J]. Acta Petrologica Sinica, 2005, 21(3):737-748. 通讯作者: 张彦龙(1983),男,副教授,主要从事火成岩岩石学方面研究.E-mail:zhangyanlong@jlu.edu.cn