世界地质    2017 36 (2): 361-370   ISSN: 1004-5589  CN: 22-1111/P  

大兴安岭北段呼中西部塔木兰沟组火山岩年代学、岩石地球化学特征及其构造意义
杨乃峰1, 杨李汀2
1. 黑龙江省矿业集团有限责任公司, 哈尔滨 150036;
2. 黑龙江省地质矿产测试应用研究所, 哈尔滨 150036
收稿日期 2016-09-29  修回日期 2017-03-27  网络版发布日期 null
参考文献  

[1] 赵忠华, 孙德有, 苟军, 等. 满洲里南部塔木兰沟组火山岩年代学与地球化学[J]. 吉林大学学报:地球科学版, 2011, 41(6):1865-1880. ZHAO Zhong-hua, SUN De-you, GOU Jun, et al. Chronology and geochemistry of volcanic rocks in Tamulangou Formation from southern Manchuria, Inner-Mongolia[J]. Journal of University: Earth Science Edition, 2011, 41(6):1865-1880.
[2] FAN Wei-ming,GUO Feng,WANG Yue-jun, et al. Late Mesozoic calc-alkaline volcanism of post-orogenic extension in the northern Da Hinggan Mountsins northeastern China[J]. Journal of Volcanology and Geothermal Reserch, 2003, 121:115-135.
[3] WANG Fei, ZHOU Xin-hua, ZHANG Lian-chang, 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, 251:179-198.
[4] 葛文春. 大兴安岭中生代火山岩的地球化学特征及其大地构造背景:博士学位论文[D]. 长春:长春科技大学, 1997. GE Wen-chun. Geochemical characteristics and geotectonic background of the volcanic rocks in Da Hinggan, NE China: doctor's degree thesis[D]. Changchun: Changchun University of Science and Technology, 1997.
[5] 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. Geochemistry of Mesozoic volcanic rocks in Da Hinggan Ling: the bimodal volcanic rocks[J]. Geochhimica, 2003, 32(3): 208-222.
[6] 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. Tectonic significance of Mesozoic volcanic rock in northeastern China[J]. Chinese Journal of Geology, 1998, 33(2): 129-139.
[7] 陈志广, 张连昌, 周新华, 等. 满洲里新右旗火山岩剖面年代学和地球化学特征[J]. 岩石化学, 2006, 22(12):2971-2986. CHEN Zhi-guang, ZHANG Lian-chang, ZHOU Xin-hua, et al. Geochronology and geochemical characteristics of volcanic rocks section in Manzhouli Xinyouqi, Inne Mongolia[J]. Acta Petrologica Sinica, 2006, 22(12): 2971-2986.
[8] 许文良, 葛文春, 裴福平, 等. 东北地区中生代火山岩作用的年代学格架及构造意义[J]. 矿物岩石地球化学通报, 2008, 27(增刊): 286-287. XU Wen-liang, GE Wen-chun, PEI Fu-ping, et al. Geochronogical framework and tectonic implication of Mesozoic volcanism in Northeast China[J]. Bulletin of Mineralogy, Petrology snd Geochemistry, 2008, 27(Suppl.): 286-287.
[9] 张连昌, 陈志广, 周新华, 等. 大兴安岭根河地区早白垩世火山岩深部源区与构造-岩浆深化: Sr-Nd-Pb-Hf同位素地球化学制约[J]. 岩石学报, 2007, 23(11): 2823-2835. ZHANG Lian-chang, CHEN Zhi-guang, ZHOU Xin-hua, et al. Characteristics of deep sources and tectonic magmatic evolution of the Early Cretaceous volcanic in Genhe area, Da Hinhgan Mountains: constraints of Sr-Nd-Pb-Hf isotopic geochemistries[J]. Acta Petrologica Sinica, 2007, 23(11):2823-2835.
[10] 赵国龙, 杨桂林, 王忠. 大兴安岭中南部中生代火山岩[M]. 北京: 北京科学技术出版社, 1989:1-260. ZHAO Guo-long, YANG Gui-lin, WANG Zhong. Mesozoic volcanic rocks in the Middle-South Da Xing'an Ling[M]. Beijing: Beijing Science and Technology Press, 1989:1-260.
[11] 孙德有, 许文良, 周燕. 大兴安岭中生代火山岩的形成机制[J]. 矿物岩石地球化学通报, 1994, 12(3): 162-164. SUN De-you, XU Wen-liang, ZHOU Yan. Forming mechanism of the Mesozoic volcanic rocks in Da Hinggan Mountain, NE China[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 1994, 12(3): 162-164.
[12] 张吉衡.大兴安岭中生代火山岩年代学及地球化学研究:博士学位论文[D]. 武汉:中国地质大学,2009. ZHANG Ji-heng. Chronology and geochemistry of the Mesozoic volcanic rocke Great Xing'an Range, northeastern China: doctor's degree thesis [D]. Wuhan: China University of Geosciences, 2009.
[13] 蒋国源, 权恒. 大兴安岭根河—海拉尔盆地中生代火山岩[J]. 中国地质科学院沈阳地质矿产研究所所刊, 1988(3):23-100. JIANG Guo-yuan, QUAN Heng. Mesozoic volcanic rocks of Genhe and Hailar basins in Da Hinggan Ling range[J]. Shenyang Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, 1998(3):23-100.
[14] 邓晋福, 赵海玲, 莫宣学, 等, 中国大陆根-柱构造-大陆动力学钥匙[M]. 北京: 地质出版社, 1996:1-100. DENG Jin-fu, ZHAO Hai-ling, MO Xuan-xue, et al. The key of continental root-column tectonic dynamic, China[M]. Beijing: Geological Publishing House, 1996:1-100.
[15] 张玉涛. 大兴安岭北段漠河地区塔木兰沟组火山岩地球化学特征[J]. 科技导报, 2013, 31(33): 25-30. ZHANG Yu-tao. Geochrmistry of Tamulangou Formation volcanic rocks in Mohe, North Da Hinggan Mountains[J]. Science & Technology Review, 2013, 31(33): 25-30.
[16] 张昱, 赵焕力, 韩彦东. 大兴安岭北段塔木兰沟组玄武岩地球化学及构造背景[J]. 地质与资源,2005, 14(2):87-96. ZHANG Yu,ZHAO Huan-li,HAN Yan-dong. Geochemical characteristics and tectonic background of basalt from Tamulangou Formation in northern Daxinganling[J]. Geolong and Resourees, 2005, 14(2):87-96.
[17] 张昱, 赵焕力, 李仰春, 等. 大兴安岭北段根河地区早白垩世火山杂岩特征及成因探讨[J].中国地质, 2005, 32(3):405-410. ZHANG Yu, ZHAO Huan-li, LI Yang-chun, et al. Characteristics of Early Cretaceous volcanic complexes in the Genhe area in the northern segment of the Da Hinggan Mountains: with a discussion of their genesis[J]. Geology in China, 2005, 32(3):405-410.
[18] 张玉涛, 张连昌, 英基丰, 等. 大兴安岭北部扎兰屯脉岩群的地球化学特征及地质意义[J]. 岩石学报, 2006, 22(11):2733-2742. ZHANG Yu-tao, ZHANG Lian-chang,YING Ji-feng, et al. Geochemistry of Zhalantun dyke swarm in north Da Hinggan Mountain and its geological implication[J].Acta Petrologiea Sinica,2006,22(11):2733-2742.
[19] 张玉涛,张连昌,英基丰,等. 大兴安岭北段塔河地区早白垩世火山岩地球化学及源区特征[J]. 岩石学报, 2007, 23(11):2811-2822. ZHANG Yu-tao, ZHANG Lian-chang, YING Ji-feng, et al. Geochemistry and source characteristics of Early Cretaceous volcanic rocks in Tahe, north Da Hinggan Mountain[J]. Acta Petrologiea Sinica, 2007, 23(11):2811-2822.
[20] 黑龙江省地质矿产局. 黑龙江省区域地质志[M].北京:地质出版社,1993:180-181. Heilongjiang Peovince Bureau of Geology and Mineral Resoures. Regional geology of Heilongjiang Province[M]. Beijing: Geological Publishing House, 1993: 180-181.
[21] 黑龙江省地质矿产局.黑龙江省岩石地层[M].武汉:中国地质大学出版社, 1997:142-143. Heilongjiang Province Bureau of Geology and Mineral Resoures. Lithostratigraphy of Heilongjiang Province[M]. Wuhan: China University of China Press, 1997:142-143.
[22] Belousova E A,Criffin W L,O'Reilly S Y,et al. Igneous zircon:trace element composition as an indicator of source rock type[J]. Contributions to Mineralogy and Petrology, 2002, 143:602-622.
[23] Frey F A, Green D H, Roy S D. Integrated models of basalt petrogenesis: a study of quartz tholeiites to olivine melilitites from South eastern Australia utilizing geochemical and experimental petrological data[J]. Journal of Petrology, 1978, 19(3):463-513.
[24] 尹志刚, 赵海滨, 赵寒冬,等. 大兴安岭北端塔木兰沟组玄武质岩石的地球化学特征及构造背景[J]. 地质通报, 2005, 24(9):848-853. YIN Zhi-gang, ZHAO Hai-bin, ZHAO Han-dong, et al. Geochemical characteristics and tectonic setting of basaltic rocks of the Tamulangou Formation at the northern end of the Da Hinggan Mountains, China[J]. Geological Bulletin of China, 2005, 24(9): 848-853.
[25] 杨乃峰. 黑龙江省飞虎山幅、1248高地幅1/5万区域地质矿产调查报告[C]. 哈尔滨:黑龙江省地球物理勘察院,2011:21-160 YANG Nai-feng. The report of 1∶500 00 area geology and mineral resources survey in Huojihe Tree Farm, Erlongshan Tree Farm, Tanghongling Tree Farm in Yichun City,Heilongjiang Province[C]. Harbin:Heilong-jiang Institute of Geophysical Exploration, 2011:21-160.
[26] 张树玉, 王方正. 玄武岩在研究岩石圈深部过程及构造背景中的应用[J]. 地球化学进展, 2002, 17(5):685-692. ZHANG Shu-yu, WANG Fang-zheng. Basalt's action on research geosphere deep-course and structural setting[J]. Advances in Earth Sciences, 2002, 17(5):685-692.
[27] 郑永飞, 李曙光, 陈江峰. 化学地球动力学[M]. 北京:科学出版社, 1999:119-167. ZHENG Yong-fei, LI Shu-guang, CHEN Jiang-feng. Chemical geodynamics[M]. Beijing: Science Press, 1999:119-167.


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