GEOCHEMICAL CHARACTERISTICS OF UPPER JURASSIC INTERMEDIATE-GRANITIC VOLCANIC ROCKS FROM NORTHERN CHIFENG, INNER MONGOLIA

HAO Bin; YANG Xin-de; ZHANG Ming-yang; XIE Cheng-fei

Volume 17 Issue 3

Sep. 2011

Turn off MathJax

Article Contents

Article Navigation > Journal of Geomechanics > 2011 > 17(3): 274-285

HAO Bin, YANG Xin-de, ZHANG Ming-yang, et al., 2011. GEOCHEMICAL CHARACTERISTICS OF UPPER JURASSIC INTERMEDIATE-GRANITIC VOLCANIC ROCKS FROM NORTHERN CHIFENG, INNER MONGOLIA. Journal of Geomechanics, 17 (3): 274-285.

Citation:

PDF( 978 KB)

GEOCHEMICAL CHARACTERISTICS OF UPPER JURASSIC INTERMEDIATE-GRANITIC VOLCANIC ROCKS FROM NORTHERN CHIFENG, INNER MONGOLIA

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Institute of Geomechanics, Chinese Academy of Geological Sciencses, Beijing 100081, China

More Information

Received: 2011-04-20
Published: 2011-09-01

Abstract

Abstract

Upper Jurassic intermediate-granitic volcanic rocks from northern Chifeng lie in Mongolia Paleo-uplift, the northern margin of the North China Craton.The lava mainly consists of rhyolite, andesite and augite andesite.The geochemical study for intermediate-granitic volcanic rocks suggests that the SiO₂ is in 50.74% ~58.82%, Al₂O₃ and K₂O+Na₂O range from 15.32% ~ 17.17% and 4.89%~7.05%, Mg^# changes from 0.13 to 0.39, which belong to Sodium and Calc-alkaline series.Geochemical results for rhyolite indicate that the SiO₂ are in 74.68%~74.86%, Al₂O₃ and K₂O+Na₂O range from 12.09%~13.13%, Mg^# changes from 0.13 to 0.39 and they belong to Calc-alkaline series or Shoshonitic series.The trace elements analysis for intermediate volcanic rocks demonstrate the insignificantly Eu anomalies (Eu^*/Eu=0.94~1.12) and intense fractionation between LREE and HREE, [(La/Yb)_N=9.6~16.09].The primitive mantle-normalized spider diagrams are characterized by LILE enrichment and HFSE depletion, especially an obviously negative Nb-Ta anomalies, and obviously positive Pb anomalies.Rhyolite has the similar characteristics and is characterized by a significantly negative Eu anomalies, [(La/Yb)_N=7.86~10.05].Based on the previous studies, we infer that intermediate volcanic rocks formed under the stretching and thinning environment.With geothermal gradient increasing and atmosphere upwelling, andesitic magma resulted from partial melting of enriched lithospheric mantle.
- intermediate-granitic volcanic rock,
- Upper Jurassic,
- lithospheric mantle,
- stretching and thinning,
- northern Chifeng

FullText(HTML)

References(37)

References

[1]	Kuzmin M L, Abramovich G Y A, Dril S L, et al. The Mongolian-Okhotsk suture as the evidence of late Paleozoic-Mesozoic collisional processes in Central Asia[C]//Abstract of 30^th IGC. Beijing: Geological Publishing House, 1996: 261.
[2]	Zhao X, Coe R S, Gilder S A, et al. Paleomagnetic constraints on the palegeography of China: Implications for Gondwanaland[J]. Australian Journal of Earth Sciences, 1996, 43: 643~672. doi: 10.1080/08120099608728285
[3]	李思田, 杨世恭.中国东北部晚中生代裂馅作用和东北亚断馅盆地系[J].中国科学: B辑, 1987, 21 (2):185~195. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jbxk198702009&dbname=CJFD&dbcode=CJFQ LI Si-tian, YANG Shi-gong. The late Mesozoic rifting in the northeastern China and the fault-rifting basins in East Asia [J]. Science in China: Series B, 1987, 21 (2):185~195. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jbxk198702009&dbname=CJFD&dbcode=CJFQ
[4]	邵济安, 藏绍先, 牟保磊.造山带的伸展构造与软流圈隆起:以兴蒙造山带为例[J].科学通报, 1994, 39 (6):533~537. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kxtb199406016&dbname=CJFD&dbcode=CJFQ SHAO Ji-an, ZANG Shao-xian, MOU Bao-lei. Extensional tectonics and asthenospheric upwelling in the orogenic belt: A case study from Hinggan-Mongolia Orogenic belt[J]. Chinese Science Bulletin, 1994, 39 (6):533~537. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kxtb199406016&dbname=CJFD&dbcode=CJFQ
[5]	徐公愉.大兴安岭的大陆火山岩及其矿化作用[J].中国区域地质, 1983, 5: 39~50. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zqyd198303004&dbname=CJFD&dbcode=CJFQ XU Gong-yu. Continental volcanic rocks in the Greater Khingan Mountains and their mineralization[J]. Geological Bulletin of China. 1983, 5: 39~50. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zqyd198303004&dbname=CJFD&dbcode=CJFQ
[6]	赵国龙, 扬桂林, 傅嘉有.大兴安岭中南部中生代火山岩[M].北京:科学出版社, 1989: 1~252. ZHAO Guo-long, YANG Gui-lin, FU Jia-you. Mesozoic volcanic rocks in central and southern Greater Khingan Mountains [M]. Beijing: Science Press, 1989: 1~252.
[7]	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, MOU Bao-lei. Tectono-thermal evolution of the middle-south section of Da Hinggan Mountains[J]. Science in China: Series D, 1998, 28 (3):193~200.
[8]	林强, 葛文春, 孙德有, 等.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. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzkx802.000&dbname=CJFD&dbcode=CJFQ LIN Qiang, GE Wen-chun, SUN De-you, et al. Tectonic significance of Mesozoic volcanic rocks in Northeastern China [J]. Scientia Geologica Sinica, 1998, 33 (2):129~139. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzkx802.000&dbname=CJFD&dbcode=CJFQ
[9]	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):396~407. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb199903007&dbname=CJFD&dbcode=CJFQ GE Wen-chun, LIN Qiang, SUN De-you, et al. Geochemical characteristics of the Mesozoic basalts in Da Hinggan Ling: Evidence of the mantle crust interaction[J]. Acta Petrologica Sinica, 1999, 15 (3):396~407. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb199903007&dbname=CJFD&dbcode=CJFQ
[10]	黄华, 高山, 胡兆初, 等.辽西彰武地区中生代高镁安山岩地球化学及其对新生下地壳拆沉作用的指示[J].中国科学: D辑, 2007, 37 (10):1287~1300. http://d.wanfangdata.com.cn/Periodical/zgkx-cd200710002 HUANG Hua, GAO shan, HU Zhao-chu, et al. Geochemical of Mesozoic high-magnesium andesite and its indication for delamination of newly formed lower crust in Zhangwu area, Western Liaoning[J]. Science in China: Series D, 2007, 37 (10):1287~1300. http://d.wanfangdata.com.cn/Periodical/zgkx-cd200710002
[11]	蒋国源, 权恒.大兴安岭、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. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ198800019003.htm JIANG Guo-yuan, QUAN Heng. Mesozoic volcanic rocks of Genhe and Hailar basins in Da Hinggan Ling Range[J]. Journal of Shenyang Institute of Geologic and Mineral Resources, Chinese Academy of Geologic Science, 1988, 3: 23~100. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ198800019003.htm
[12]	周新华, 张国辉, 杨进辉, 等.华北克拉通北缘晚中生代火山岩Sr-Nd-Pb同位素填图及其构造意义[J].地球化学, 2001, 30 (1):10~23. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqhx200101003 ZHOU Xin-hua, ZHANG Guo-hui, YANG Jin-hui, et al. Sr-Nd-Pb isotope mapping of Late Mesozoic volcanic rocks across northern margin of North China Craton and implications to geodynamic processes[J]. Geochimica, 2001, 30 (1):10~23. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqhx200101003
[13]	吴利仁.华东及邻区中、新生代火山岩[M].北京:科学出版社, 1984: 1~286. WU Li-ren. The Mesozoic-Cenozoic Volcanic Rocks in Eastern China and Its Vincinity[M]. Beijing: Science Press, 1984: 1~286.
[14]	徐义刚, 李洪颜, 庞崇进, 等.论华北克拉通破坏的时限[J].科学通报, 2009, 59 (14):1974~1989. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kxtb200914005&dbname=CJFD&dbcode=CJFQ XU Yi-gang, LI Hong-yan, PANG Chong-jin, et al. On the timing and duration of the destruction of the North China Craton. Chinese Science Bulletin, 2009, 59 (14):1974~1989. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kxtb200914005&dbname=CJFD&dbcode=CJFQ
[15]	王忠, 朱洪森.大兴安岭中南段中生代火山岩特征及演化[J].中国区域地质, 1999, 18 (4):1~8. http://www.cqvip.com/Main/Detail.aspx?id=3874570 WANG Zhong, ZHU Hong-sen. Temporal and spatial evolution of the Mesozoic volcanism in mid southern Daxinganling Mountain[J]. Regional Geology of China, 1999, 18 (4):1~8. http://www.cqvip.com/Main/Detail.aspx?id=3874570
[16]	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. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200101017 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 Petrologica Sinica, 2001, 17 (1):161~168. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200101017
[17]	Boynton W V. Geochemistry of the rare earth elements: meteorite studies[C]//Henderson P. Rare earth element geochemistry. Netherlands: Elsevier, 1984: 63~114.
[18]	Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts: implication for mantle composition and processes[C]//Saunder A D, Norry M J. Magmatism in the ocean basins. London: Geological Society, 1989: 313~345. https://academic.oup.com/petrology
[19]	侯增谦, 罗再文.三江地区义敦岛弧安山岩成因[J].岩石矿物学杂志, 1992, 11 (1):1~14. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=yskw199201000&dbname=CJFD&dbcode=CJFQ HOU Zeng-qian, LUO Zai-wen. Origin of the andesite in Yidun island arc, Sanjiang region[J]. Acta Petrologica Et Mineralogica, 1992, 11 (1):1~14. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=yskw199201000&dbname=CJFD&dbcode=CJFQ
[20]	Grove T L, Bryan W B. Fractionation of pyroxene-phyric MORB at low pressure: An experimental study[J]. Contributions to Mineralogy and Petrology, 1983, 84 (4):293~309. doi: 10.1007/BF01160283
[21]	Grove TL, Baker M B. Phase equilibrium control on the tholeiitic versus calcalkaline diffentiation trends[J]. Journal of Geophysical Research, 1984, 89: 3253~3274. doi: 10.1029/JB089iB05p03253
[22]	吴英华, 张连昌, 周新华, 等.大兴安岭中段晚中生代安山岩年代学和地球化学特征及成因分析[J].岩石学报, 2008, 24 (6):1339~1352. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200806018&dbname=CJFD&dbcode=CJFQ WU Ying-hua, ZHANG Lian-chang, ZHOU Xin-hua, et al. Geochronology and Geochemical characteristics of Late Mesozoic andesites in the Central Da-Hinggan Mountains, and its genesis[J]. Acta Petrologica Sinica, 2008, 24 (6):1339~1352. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200806018&dbname=CJFD&dbcode=CJFQ
[23]	Rapp R P, Shimizu N, Norman M D, et al. Reaction between slab-derived melts and peridotite in the mantle wedge: Experimental constraints at 3. 8 GPa[J]. Chemical Geology, 1999, 160 (4):335~356. doi: 10.1016/S0009-2541(99)00106-0
[24]	Xu Y G. Thermo-tectonic destruction of the Archaean lithospheric keel beneath the Sino-Korean Craton in china: evidence, timing and mechanism[J]. Physics and Chemistry of the Earth (A), 2001, 26 (9-10):747~757. doi: 10.1016/S1464-1895(01)00124-7
[25]	吴福元, 徐义刚, 高山, 等.华北岩石圈减薄与克拉通破坏研究的主要学术争论[J].岩石学报, 2008, 24: 1145~1174. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200806001 WU Fu-yuan, XU Yi-gang, GAO Shan, et al. Lithospheric thinning and destruction of the North China Craton[J]. Acta Petrologica Sinica, 2008, 24: 1145~1174. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200806001
[26]	路凤香, 桑隆康.岩石学[M].北京:地质出版社, 2002: 90~101. LU Feng-xiang, SANG Long-kang. Petrology[M]. Beijing: Geological Publishing House, 2002: 90~101.
[27]	Engebretson D C, Cox A, Gordon R G. Relative motions between oceanic and continental plates in the Pacific basins [J]. Geological Society of America Special Paper, 1985, 206: 1~59. doi: 10.1130/SPE206
[28]	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. http://d.wanfangdata.com.cn/Periodical/gjsdz200502002 ZHANG Yu, ZHAO Huan-li, HAN Yan-dong. Geochemical characteristics and tectonic background of basalt from Tamulangou Formation in northern Daxinanling[J]. Journal of Precious Metallic Geology, 2005, 14 (2):87~96. http://d.wanfangdata.com.cn/Periodical/gjsdz200502002
[29]	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].岩石学报, 2006, 22 (12):1~14. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200612014 CHEN Zhi-Guang, ZHANG Lian-chang, ZHOU Xin-hua, et al. Geochronology and geochemical characteristics of volcanic rocks section in Manzhouli Xinyouqi, Inner Mong olia[J]. Acta Geologica Sinica, 2006, 22 (12):1~14. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200612014
[30]	葛文春, 林强, 李献华, 等.大兴安岭北部伊列克得组玄武岩的地球化学特征[J].矿物岩石, 2000, 20 (3):14~18. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwys200003003 GE Wen-chun, LIN Qiang, LI Xian-hua, et al. Geochemical characteristics of basalts of the early Cretaceous Yiliekede formation, North Daxing' anling[J]. Journal of Mineralogy and Petrology. 2000, 20 (3):14~18. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwys200003003
[31]	张拴宏, 赵越, 刘建民, 等.华北地块北缘晚古生代—早中生代岩浆活动期次、特征及构造背景[J].岩石矿物学杂志, 2010, 29 (6):824~842. http://www.cqvip.com/Main/Detail.aspx?id=35849260 ZHANG Shuan-hong, ZHAO Yue, LIU Jian-Min, et al. Geochronology, geochemistry and tectonic setting of the Late Paleozoic-Early Mesozoic magmatism in the northern margin of the North China Block: A preliminary review[J]. Acta Petrologica Et Mineralogica, 2010, 29 (6):824~842. http://www.cqvip.com/Main/Detail.aspx?id=35849260
[32]	张宏福, 周新华, 范蔚茗, 等.华北东南部中生代岩石圈地慢性质、组成、富集过程及其形成机理[J].岩石学报, 2005, 21 (4):1271~1280. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200504024&dbname=CJFD&dbcode=CJFQ ZHANG Hong-fu, ZHOU Xin-hua, FAN Wei-ming, et al. Nature, composition, enrichment processes and its mechanism of the Mesozoic lithospheric mantle beneath the southeastern North China Craton[J]. Acta Petrologica Sinica, 2005, 21 (4):1271~1280. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200504024&dbname=CJFD&dbcode=CJFQ
[33]	韩宝福, 王式.赤峰地区新生代玄武岩的基本特征及成因[J].北京大学学报:自然科学版, 1998, 34 (1):88~96. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=bjdz801.013&dbname=CJFD&dbcode=CJFQ HAN Bao-fu, WANG Shi. General features and origin of Cenozoic basalts from Chifeng region, North China[J]. Acta Scicentiarum Naturalum Universitis Pekinesis, 1998, 34 (1):88~96. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=bjdz801.013&dbname=CJFD&dbcode=CJFQ
[34]	贾文, 朱慧忠, 邵济安.内蒙古赤峰地区新生代玄武岩的时空分布[J].地质论评, 2002, 48 (3):267~272. http://www.cqvip.com/Main/Detail.aspx?id=6194136 JIA Wen, ZHU Hui-zhong, SHAO Ji-an. Temporal-Spatial distribution of Cenozoic basalts in Chifeng area, Inner Mongolia[J]. Geological Review, 2002, 48 (3):267~272. http://www.cqvip.com/Main/Detail.aspx?id=6194136
[35]	国家地震局《深物探成果鉴定》编写组.中国地壳上地幔地球物理探测成果[M].北京:地震出版社, 1986: 1~407. Edition Group of Deep Geophysical Results Drafting, State Seismology Bureau. The geophysical exploration results of crust and upper mantle in China[M]. Beijing: Seismological Publishing House. 1986: 1~407.
[36]	徐义刚.用玄武岩组成反演化中—新生代华北岩石圈的演化[J].地学前缘, 2006, 13: 93~104. doi: 10.3321/j.issn:1005-2321.2006.02.008 XU Yi-gang. Using basalt geochemistry to constrain Mesozoic-Cenozoic evolution of the lithosphere beneath North China Craton[J]. Earth Science Frontiers, 2006, 13: 93~104. doi: 10.3321/j.issn:1005-2321.2006.02.008
[37]	路凤香, 郑建平, 邵济安, 等.华北东部中生代晚期-新生代软流圈上涌与岩石圈减薄[J].地学前缘, 2006, 13: 86~92. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dxqy200602009&dbname=CJFD&dbcode=CJFQ LU Feng-xiang, ZHENG Jian-ping, SHAO Ji-an, et al. Asthenospheric upwelling and lithospheric thinning in late Cretaceous-Cenozoic in eastern North China[J]. Earth Science Frontiers, 2006, 13: 86~92. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dxqy200602009&dbname=CJFD&dbcode=CJFQ