世界地质    2019 38 (4): 921-930   ISSN: 1004-5589  CN: 22-1111/P  

大兴安岭中段罕达盖地区早白垩世花岗岩的成因及其地质意义
贾海明1, 景妍2, 王清海3, 兰丽雪2, 井佳浩2
1. 吉林省地质调查院, 长春 130102;
2. 吉林大学 地球科学学院, 长春 130061;
3. 吉林大学 东北亚国际地学研究与教学中心, 长春 130026
收稿日期 2019-11-15  修回日期 2019-12-05  网络版发布日期 null
参考文献  [1] Wu F Y, Yang Y H, Xie L W, et al. Hf isotopic compo-sitions of the standard zircons in U-Pb geochronology[J]. Chemical Geology, 2006, 234(1/2):105-126.
[2] Şengör A M C, Natal'In B A, Burtman V S. Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia[J]. Nature, 1993, 364:299-307.
[3] 许文良, 孙德有, 尹秀英. 大兴安岭海西期造山带的演化:来自花岗质岩石的证据[J]. 长春科技大学学报, 1999, 29(4):319-323. XU Wen-liang, SUN De-you, YIN Xiu-ying. Evolution of Hercynian orogenic belt in Daxing'anling Mt:evidence from granitic rocks[J]. Journal of Changchun University of Science and Technology, 1999, 29(4):319-323.
[4] 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.
[5] 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:Geo-logical Publishing House, 1991:1-725.
[6] 赵芝. 大兴安岭北部晚古生代岩浆作用及其构造意义:博士学位论文[D]. 长春:吉林大学, 2011. ZHAO Zhi. Late Paleozoic magmatism and its tectonic significance in the northern Great Xing'an Range, north-eastern China:doctor's degree thesis[D]. Changchun:Jilin University, 2011.
[7] 孙巍, 迟效国, 潘世语, 等. 大兴安岭北部新林地区倭勒根群大网子组锆石LA-ICP-MS U-Pb年龄及其地质意义[J]. 吉林大学学报(地球科学版), 2014, 44(1):176-185. SUN Wei, CHI Xiao-guo, PAN Shi-yu, et al. Zircon LA-ICP-MS U-Pb dating and its geological significance of the Dawangzi Formation from Wolegen Group in Xinlin ar-ea, northern Great Xing'an Range[J]. Journal of Jilin University (Earth Science Edition), 2014, 44(1):176-185.
[8] Andersen T. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2002, 192(1/2):59-79.
[9] Wu F Y, Lin J Q, Wilde S A, et al. Nature of signifi-cance of the Early Cretaceous giant igneous event in east-ern China[J]. Earth and Planetary Science Letters, 2005, 233(1/2):103-119.
[10] Koschek G. Origin and significance of the SEM cath-odoluminescence from zircon[J]. Journal of Microsco-py, 1993, 171(3):223-232.
[11] Belousova E, Griffin W L, O'Reilly S Y, et al. Igneous zircon:trace element composition as an indicator of source rock type[J]. Contribution to Mineralogy and Petrology, 2002, 143(5), 602-622.
[12] Maniar P D, Piccoli P M. Tectonic discrimination of granitoids[J]. Geological Society of American Bulle-tin, 1989, 101(5):635-643.
[13] Irvine T N, Baragar W R A. A guide to the chemical classification of the common volcanic rocks[J]. Cana-dian Journal of Earth Sciences, 1971, 8(5):523-548.
[14] Peccerillo A, Taylor S R. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, north-ern Turkey[J]. Contributions to Mineralogy and Petrol-ogy, 1976, 58(1):63-81.
[15] Boynton W V. Geomochemistry of the rare earth ele-ments:meteorite studies[M]//Henderson P. Rare earth elements geochemistry. Amsterdam:Elsevier, 1984:63-114.
[16] Sun S, McDonough W F. Chemical and isotopic system-atics of oceanic basalts:implications for mantle composi-tion and processes[J]. Geological Society, London, Special Publications, 1989, 42(1):313-345.
[17] 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.
[18] 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:con-straints from geochronology, geochemistry and zircon Hf isotopes[J]. Journal of Asian Earth Sciences, 2016, 115:228-246.
[19] 于倩. 兴安地块晚古生代-早中生代侵入岩的成因及其地质意义:博士学位论文[D]. 长春:吉林大学, 2017. YU Qian. Petrogenesis of the Late Paleozoic-Early Mes-ozoic intrusive rocks in the Xing'an terrane, and its geo-logical implication:doctor's degree thesis[D]. Chang-chun:Jilin University, 2017.
[20] 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 Mes-ozoic 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.
[21] 李宇. 兴安地块中生代火成岩的年代学与地球化学:对蒙古-鄂霍茨克构造体系演化的制约:博士学位论文[D]. 长春:吉林大学, 2018. LI Yu. Geochronology and geochemistry of the Mesozoic igneous rocks in the Xing'an massif, NE China:con-straints on the evolution of the Mongol-Okhotsk tectonic regime:doctor's degree thesis[D]. Changchun:Jilin University, 2018.
[22] 谢健. 大兴安岭中段五岔沟地区早白垩世花岗质岩石的地球化学特征及其成因:硕士学位论文[D]. 长春:吉林大学, 2017. XIE Jian. Geochemical characteristics and petrogenesis of Early Cretaceous granitoids in Wuchagou region of central Great Xing'an Range:master's degree thesis[D]. Changchun:Jilin University, 2017.
[23] Chappell B W, White A J R. Two contrasting granite types[J]. Pacific Geology, 1974, 8(2):173-174.
[24] Shao J, Zhang L, Mu B L. Tectono-thermal evolution of middle-south section of the Da Hinggan Mountains[J]. Science in China (Ser. D), 1998, 41(6):570-579.
[25] 林强, 葛文春, 孙德有, 等. 中国东北地区中生代火山岩的大地构造意义[J]. 地质科学, 1998, 33(2):129-139. LIN Qiang, GE Wen-chun, SUN De-you, et al. Tecton-ic significance of Mesozoic volcanic rocks in northeastern China[J]. Chinese Journal of Geology, 1998, 33(2):129-139.
[26] 林强, 葛文春, 曹林, 等. 大兴安岭中生代双峰式火山岩的地球化学特征[J]. 地球化学, 2003, 32(3):208-222. LIN Qiang, GE Wen-chun, CAO Lin, et al. Geochem-istry of Mesozoic volcanicr ocks in Da Hinggan Ling:the bimodal volcanic rocks[J]. Geochimica, 2003, 32(3):208-222.
[27] 邵济安, 张履桥, 牟保磊. 大兴安岭中南段中生代的构造热演化[J]. 中国科学(D辑), 1998, 28(3):193-200. SHAO Ji-an, ZHANG Lü-qiao, MU Bao-lei. Mesozoic tectono-thermal evolution of the Da Hinggan Ling[J]. Science in China (Ser. D) 1998, 28(3):193-200.
[28] 邵济安, 赵国龙, 王忠, 等. 大兴安岭中生代火山活动构造背景[J]. 地质论评, 1999, 45(增刊1):422-430. SHAO Ji-an, ZHAO Guo-long, WANG Zhong, et al. Tectonic setting of Mesozoic volcanism in Da Hinggan Mountains, northeastern China[J]. Geological Review, 1999, 45(Suppl. 1):422-430.
[29] 邵济安, 刘福田, 陈辉, 等. 大兴安岭-燕山晚中生代岩浆活动与俯冲作用关系[J]. 地质学报, 2001, 75(1):56-63. SHAO Ji-an, LIU Fu-tian, CHEN Hui, et al. Relation-ship between Mesozoic magmatism and subduction in Da hinggan-Yanshan area[J]. Acta Geologica Sinica, 2001, 75(1):56-63.
[30] 葛文春, 林强, 孙德有, 等. 大兴安岭中生代玄武岩的地球化学特征:壳幔相互作用的证据[J]. 岩石学报, 1999, 15(3):396-406. GE Wen-chun, LIN Qiang, SUN De-you, et al. Geo-chemical characteristics of the Mesozoic basalts in Da Hinggan Ling:evidence of the mantle-crust interaction[J]. Acta Petrologica Sinica, 1993, 15(3):396-406.
[31] 葛文春, 林强, 孙德有, 等. 大兴安岭中生代两类流纹岩成因的地球化学研究[J]. 地球科学, 2000, 25(2):172-178. GE Wen-chun, LIN Qiang, SUN De-you, et al. Geo-chemical research into origins of two types of Mesozoic rhyolites in Daxing'anling[J]. Earth Science, 2000, 25(2):172-178.
[32] 葛文春, 李献华, 林强, 等. 呼伦湖早白垩世碱性流纹岩的地球化学特征及其意义[J]. 地质科学, 2001, 36(2):176-183. GE Wen-chun, LI Xian-hua, LIN Qiang, et al. Geo-chemistry of Early Cretaceous alkaline rhyolites from Hulun lake, Daxing'anling and its tectonic implications[J]. Scientia Geologica Sinica, 2001, 36(2):176-183.
[33] 郭锋, 范蔚茗, 王岳军, 等. 大兴安岭南段晚中生代双峰式火山作用[J]. 岩石学报, 2001, 17(1):161-168. GUO Feng, FAN Wei-ming, WANG Yue-jun, et al. Petrogenesis of the Late Mesozoic bimodal volcanic rocks in the southern Da Hinggan Mts, China[J]. Acta Pet-rologica Sinica, 2001, 17(1):161-168.
[34] Fan W M, Guo F, Wang Y J, et al. Late Mesozoic calc-alkaline volcanism of post-orogenic extension in the northern Da Hinggan Mountains, northeastern China[J]. Journal of Volcanology and Geothermal Research, 2003, 121(1/2):115-135.
[35] 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. Or-igin of Late Mesozoic intermediate-felsic volcanic rocks from the northern Dahinggan Mountain, NE China[J]. Acta Petrologica Sinica, 2005, 21(3):737-748.
[36] 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.
[37] Van der Voo R, Spakman W, Bijwaard H. Mesozoic subducted slabs under Siberia[J]. Nature, 1999, 397(6716):246-249.
[38] Tomurtogoo O, Windley B F, Krøner A, et al. Zircon age and occurrence of the Adaatsag ophiolite and Muron shear zone, central Mongolia:constraints on the evolu-tion of the Mongol-Okhotsk ocean, suture and orogen[J]. Journal of the Geological Society, 2005, 162(1):125-134.

通讯作者: 景妍(1995),女,硕士研究生,从事岩石学方面研究。E-mail:jingyan18@mails.jlu.edu.cn