Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (4): 1121-1131.doi: 10.13278/j.cnki.jjuese.201504115

Previous Articles     Next Articles

Early Carboniferous Tectonic Attribute of the Central-Northern Margin of North China Craton: Constraints from Geochemistry of Highly Fractionated Ⅰ-Type Granites in Cahayouhouqi Area

Liu Qun1, Wang Wanqiong2, Qiu Dianming3, Bai Xinhui4, Zhang Jinfeng4, Wang Xin4   

  1. 1. Heilongjiang Institute of Geophysical Exploration, Harbin 150036, China;
    2. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China;
    3. Editorial Department of Journal, Jilin University, Changchun 130026, China;
    4. College of Earth Science, Jilin University, Changchun 130061, China
  • Received:2014-10-21 Published:2015-07-26

PDF (PC)

495

Abstract:

This study focuses on the petrology and geochemistry of the monzonitic granites from the Cahayouhouqi area in Inner Mongolia. Tectonically it is located in the central-northern margin of the North China craton. These rocks have high content of silica, kalium and alkalis, low abundance of calcium, phosphorus, iron, magnesium; w(P2O5) decreases with the increasing of w(SiO2); A/CNK equals 0.96-1.15; and differentiation index DI is between 90.36-92.96. The granites consist mainly of perthite, plagioclase, quartz, minor biotite, no mafic alkaline minerals and Al-rich minerals; their accessory minerals are zircon, magnetite, apatite, sphene and ilmenite. Combined with the petrological and geochemical characteristics, the granites can be classified as a highly fractionated I-type granite. The low content of ∑REE ((46.8-94.4)×10-6), Th ((1.74-2.39)×10-6), and U ((0.27-0.39)×10-6), as well as their trace element discrimination diagrams indicate that the magma source derived from the lower crust, and their source-rock was lithosphere mantle. The chondrite normalized patterns are right declined with a serious positive Eu anomaly (δEu=0.83-3.51). They are enriched in the large ion lithophile elements (LILEs, e.g., Cs, Rb, Ba, and K), and depleted of the high field-strength elements (HFSEs, e.g., Nb, Ta, P, and Ti). Their geochemical characteristics indicates that the monzonitic granites emplaced in an active continental margin as a result of the Early Carboniferous subduction of Paleo-Asian Ocean towards the northern margin of the North China craton.

Key words: northern margin North China craton, Inner Mongolia, Early Carboniferous, highly fractionated I-type granites, active continental margin arc, Paleo-Asian Ocean

CLC Number: 

  • P588.12

[1] Xiao Wenjiao, Windly Brian F, Hao Jie, et al. Accretion Leading to Collision and the Permian Solonker Suture, Inner Mongolia, China: Termination of the Central Asian Orogenic Belt[J]. Tectonics, 2003, 22(6): 1069-1089.

[2] Sengör 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] Tang Kedong. Tectonic Development of Paleozoic Fol-dbelts at the North Margin of the Sino-Korean Craton[J]. Tectonics, 1990, 9(2): 249-260.

[4] 陈衍景, 翟明国, 蒋少涌. 华北大陆边缘造山过程与成矿研究的重要进展和问题[J]. 岩石学报, 2009, 25(11): 2695-2726. Chen Yanjing,Zhai Mingguo,Jiang Shaoyong.Significant Achievements and Open Issues in Study of Orogenesis and Metallogenesis Surrounding the North China Continent[J]. Acta Petrologica Sinica, 2009, 25(11): 2695-2726.

[5] 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. Zhang Shuanhong, Zhao Yue, Liu Jianmin, 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.

[6] 肖文交, 舒良树, 高俊, 等. 中亚造山带大陆动力学过程与成矿作用[J]. 新疆地质, 2008, 26(1): 5-8. Xiao Wenjiao, Shu Liangshu, Gao Jun, et al. Continental Dynamics of the Central Asian Orogenic Belt and Its Metallogeny[J]. Xinjiang Geology, 2008, 26(1): 5-8.

[7] Jahn Borming, Capdevila R, Liu Dunyi, et al. Sources of Phanerozoic Granitoids in the Transect Bayanhongor-Ulaan Baatar Mongolia: Geochemical and Nd Isotopic Evidence, and Implications for Phanerozoic Crustal Growth[J]. Journal of Asian Earth Sciences, 2004, 23: 629-653.

[8] 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: 351-458. Bureau Geology and Mineral Resources of Inner Mongolia Autonomous Region. Regional Geology of Inner Mongolia Autonomous Region[M].Beijing:Geological Publishing House, 1991: 351-458.

[9] 许立权. 内蒙古白云鄂博满都拉地区加里东期华力西期印支期岩浆岩特征与大地构造演化探讨[D]. 北京: 中国地质大学, 2005: 8-86. Xu Liquan. The Characteristics of Magmatic Rocks and Discussion of Geotectonics Evolution from Caledonian Through Hercynian to Indosinian Stage in the Baiyun'ebo-Mandula Region, Inner Mongolia[D]. Beijing: China University of Geosciences, 2005: 8-86.

[10] 张臣, 刘树文, 韩宝福, 等. 内蒙古商都大石沟花岗岩体锆石SHRIMP U-Pb 年龄及其意义[J]. 岩石学报, 2007, 23(3): 591-596. Zhang Chen, Liu Shuwen, Han Baofu, et al. SHRIMP U-Pb Dating of Dashigou Biotite-K-Felspar Granites in Shangdu, Inner Mongolia, and Its Significance[J]. Acta Petrologica Sinica, 2007, 23(3): 591-596.

[11] Zhang Shuanhong, Zhao Yue, Song Biao, et al. Carboniferous Granitic Plutons from the Northern Margin of the North China Block: Implications for a Late Palaeozoic Active Continental Margin[J]. Journal of the Geological Society, 2007, 164: 451-463.

[12] Zhang Shuanhong, Zhao Yue, Liu Xiaochun, et al. Late Paleozoic to Early Mesozoic Mafic-Ultramafic Complexes from the Northern North China Block: Constraints on the Composition and Evolution of the Lithospheric Mantle[J]. Lithos, 2009, 110: 229-246.

[13] 王挽琼, 刘正宏, 王兴安, 等. 内蒙古乌拉特中旗海西期黑云母二长花岗岩锆石SHRIMP U-Pb年龄及其地质意义[J]. 吉林大学学报:地球科学版, 2012, 42(6): 1771-1782. Wang Wanqiong, Liu Zhenghong, Wang Xing'an, et al. SHRIMP U-Pb Dating of the Zircon from the Hercynian Biotile Monzontic Granites in Urad Zhongqi, Inner Mongolia, and Its Geological Significance[J]. Journal of Jilin University:Earth Science Edition, 2012, 42(6): 1171-1782.

[14] 王挽琼, 徐仲元, 刘正宏, 等. 华北板块北缘中段早中二叠世的构造属性: 来自花岗岩类锆石U-Pb年代学及地球化学的制约[J]. 岩石学报, 2013, 29(9): 2987-3003. Wang Wanqiong, Xu Zhongyuan, Liu Zhenghong, et al. Early-Minddle Permian Tectonic Evolution of the Central-Northern Margin of the North China Craton: Constraints from Zircon U-Pb Ages and Geochemistry of the Granitoids[J]. Acta Petrologica Siniaca, 2013, 29(9): 2987-3003.

[15] Jian Ping, Liu Dunyi, Kröner Alfred, et al. Evolution of a Permian Intraoceanic Arc-Trench System in the Solonker Suture Zone, Central Asian Orogenic Belt, China and Mongolia[J]. Lithos, 2010, 118: 169-190.

[16] 柳长峰. 内蒙古四子王旗地区古生代早中生代岩浆岩带及其构造意义[D]. 北京: 中国地质大学, 2010: 111-117. Liu Changfeng. Paleozoic-Early Mesozoic Magmatic Belts and Tectonic Significance in Siziwangqi Area, Inner Mongolia[D]. Beijing: China University of Geosiences, 2010: 111-117.

[17] 陈志勇. 内蒙古固阳满都拉地区中元古代古生代地质构造演化[D]. 北京: 中国地质大学, 2005: 102-124. Chen Zhiyong. Tectonic Evolution from Middle-Proterozoic to Paleozic in Guyang-Mandula Area, Inner Monglia[D]. Beijing: China University of Geosciences, 2005: 102-124.

[18] 潘世语,迟效国,孙巍,等. 内蒙古苏尼特右旗晚石炭世本巴图组火山岩地球化学特征及构造意义[J]. 世界地质, 2012, 31(1): 40-50. Pan Shiyu, Chi Xiaoguo, Sun Wei, et al. Geochemical Characteristics and Tectonic Significance of Late Carboniferous Volcanic Rocks in Benbatu Formation of Sonid Youqi, Inner Mongolia[J]. Global Geology, 2012, 31(1): 40-50.

[19] 童英,洪大卫,王涛,等. 中蒙边境中段花岗岩时空分布特征及构造和找矿意义[J]. 地球学报, 2010, 31(3): 395-412. Tong Ying, Hong Dawei, Wang Tao, et al. Spatial and Temporal Distribution of Granitoids in the Middle Segment of the Sino-Mongolian Border and Its Tectonic and Metallogenic Implications[J]. Acta Geos-cientica Sinica, 2010, 31(3): 395-412.

[20] Boynton W V. Geochemistry of the Rare Earth Elements: Meteorite Studies//Henderson P.Rare Earth Element Geochemistry.Amsterdam:Elservier, 1984: 63-114.

[21] Sun S S, McDonough W F. Chemical and Isotopic Systematic of Oceanic Basalts: Implication for Mantle Compositions and Processes[C]//Saunder A D, Norry M J. Magmatism in the Ocean Basins.[S.I.]: Geological Society Special Publication,1989: 313-345.

[22] 魏庆国, 高昕宇, 赵太平, 等. 大别北麓汤家坪花岗斑岩锆石LA-ICPMS U-Pb定年和岩石地球化学特征及其对岩石成因的制约[J]. 岩石学报, 2010, 26(5): 1550-1562. Wei Qingguo, Gao Xinyu, Zhao Taiping, et al. Petrogenesis of Tangjiaping Granite Porphyry in Northern Dabie: Evidence from Zircon LA-ICPMS U-Pb Dating and Geochemical Characteristics[J]. Acta Petrologica Siniaca, 2010, 26(5): 1550-1562.

[23] 吴福元, 李献华, 杨进辉, 等. 花岗岩成因研究的若干问题[J]. 岩石学报, 2007, 23(6): 1217-1238. Wu Fuyuan, Li Xianhua, Yang Jinhui, et al. Discussions on the Petrogenesis of Granites[J]. Acta Petrologica Siniaca, 2007, 23(6): 1217-1238.

[24] Chappell B W. Aluminium Saturation in I and S-Type Granites and the Characterization of Fractionated Haplogranites[J]. Lithos, 1999, 46: 535-551.

[25] 李献华, 李武显, 李正祥. 再论南岭燕山早期花岗岩的成因类型与构造意义[J]. 科学通报, 2007, 52(9): 981-991. Li Xianhua, Li Wuxian, Li Zhengxiang. On the Genetic Classification and Tectonic Implications of the Early Yanshanian Granitoids in the Nanling Range, South China[J]. Chinese Science Bulletin, 2007, 52(9): 981-991.

[26] 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: 407-419.

[27] Sylvester P J. Post-Collisional Alkaline Granites[J]. Journal of Geology, 1989, 97(3): 261-280.

[28] Wu Fuyuan, Jahn Borming, Wiled S A, et al. Highly Fractionated I-Type Granites in NE China(I): Geochronology and Petrogenesis[J]. Lithos, 2003, 66: 541-573.

[29] Ionov D A,Gregoire M, Prikhod'ko V S. Feldspar-Ti-Oxide Metasomatism in Off-Cratonic Continental and Oceanic Upper Mantle[J]. Earth and Planetary Science Letters,1999, 165: 37-44.

[30] Gill J B. Orogenic Andesites and Plate Tectonics[M]. New York: Springer Verlag,1981: 385.

[31] 李昌年. 火成岩微量元素岩石学[M]. 武汉: 中国地质大学出版社, 1992: 134-135. Li Changnian. Trace Element Petrology of Igneous Rocks[M]. Wuhan: China University of Geosciences Press, 1992: 134-135.

[32] Rudnick R L, Gao S. Composition of the Continental Crust[C]//Rudniek R L. The Crust. Treatise on Ceochemistry Oxford: Elsevier Pergamon, 2003: 1-64.

[33] Pearce J A. Source and Settings of Granitic Rocks[J]. Episodes, 1996, 19(4): 120-125.

[34] Kelmen P B, Hangh K, Greenem A R. One View of the Geochemistry of Subduction-Related Magmatic Arcs, with an Emphasis on Primitive Andesite and Lower Crust[C]//Rudnick R L. Treatise on Geochemistry. Oxford: Elsevier Pergamon, 2003: 593-689.

[35] 洪大卫, 王式洸, 谢锡林, 等. 从中亚正εNd值花岗岩看超大陆演化和大陆地壳生长的关系[J]. 地质学报, 2003, 77(2): 203-209. Hong Dawei, Wang Shiguang, Xie Xilin, et al. Correlation Between Continental Crustal Growth and the Supercontinental Cycle: Evidence from the Granites with Positive εNd in the Central Asian Orogenic Belt[J]. Acta Geologica Sinica, 2003, 77(2): 203-209.

[36] Yue Yongjun, Liou J G, Graham S A. Tectonic Correlation of Beishan and Inner Mongolia Orogens and Its Implications for the Palinspastic Reconstruction of North China[J]. Geological Society of America Menoirs, 2001, 194:101-116.

[37] 徐备,陈斌.内蒙古北部华北板块与西伯利亚板块之间中古生代造山带的结构及演化[J]. 中国科学:D辑, 1997, 27(3): 227-232. Xu Bei, Chen Bin. The Structure and Evolution of a Middle Paleozoic Orogenic Belt Between the North China and Siberian Blocks, Northern Inner Mongolia, China[J].Science in China: Series D, 1997, 27(3): 227-232.

[38] 郭胜哲. 中朝板块与西伯利亚板块拼合时限的确定及其生物地层学依据[J]. 中国地质科学院沈阳地质矿产研究所, 1986, 14: 127-136. Guo Shengzhe. On Determination of Convergence Time Between Siberian Plate and Sino-Korean Plate and Its Biostratigraphic Evidence[J]. Shenyang Institute of Geology and Mineral Resources Chinese Academy of Geological Sciences,1986,14:127-136.

[39] Hong Dawei, Huang Huaizeng, Xiao Yijun, et al. Permian Alkaline Granites in Central Inner Mongolia and Their Geodynamic Significance[J]. Acta Geologica Sinica, 1995, 8(1): 27-39.

[40] Zhang Xiaohui, Zhang Hongfu, Tang Yanjie, et al. Geochemistry of Permian Bimodal Volcanic Rocks from Central Inner Mongolia, North China: Implication for Tectonic Setting and Phanerozoic Continental Growth in Central Asian Orogenic Belt[J]. Chemical Geology, 2008, 249: 262-281.

[41] Xiao Wenjiao, Windley B F, Huang B C, et al. End-Permian to Mid-Triassic Termination of Accretionary Processes of the Southern Altaids: Implications for the Geodynamic Evolution, Phanerozoic Continental Growth, and Metallogeny of Central Asia[J]. International Journal of Earth Sciences, 2009, 98: 1189-1217.

[42] 孙德有, 吴福元, 张艳斌, 等. 西拉木伦河长春延吉板块缝合带的最后闭合时间:来自吉林大玉山花岗岩体的证据[J]. 吉林大学学报:地球科学版, 2004, 34(2): 174-181. Sun Deyou, Wu Fuyuan, Zhang Yanbin, et al. The Final Closing Time of the West Lamulun River-Changchun-Yanji Plate Suture Zone:Evidence from the Dayushan Granite Pluton, Jilin Province[J]. Journal of Jilin University:Earth Science Edition, 2004, 34(2): 174-181.

[43] Li Jinyi. Permian Geodynamic Setting of Northeast China and Adjacent Regions: Closure of the Paleo-Asian Ocean and Subduction of the Paleo-Pacific Plate[J]. Journal of Asian Earth Sciences, 2006, 26: 207-224.

[44] 赵越,陈斌,张拴宏,等. 华北克拉通北缘及邻区前燕山期主要地质事件[J]. 中国地质, 2010, 37(4): 900-915. Zhao Yue, Chen Bin, Zhang Shuanhong, et al. Pre-Yanshanian Geological Events in the Northern Margin of North China Craton and Its Adjacent Areas[J]. Geology China, 2010, 37(4): 900-915.

[45] 陈斌. 内蒙古兴安地区二叠系沉积特征及构造背景[D]. 北京: 中国地质大学, 2011:30-53. Chen Bin. Sedimentary Characteristics and Tectonic Setting of Permian in Xing'an Region of Inner Mongolian Autonomous Region[D]. Beijing: China University of Geosciences, 2011: 30-53.

[46] 范振华,李绪俊,梁本胜,等. 吉林安图海沟岩体岩石地球化学特征及其成岩构造环境[J]. 世界地质,2012, 31(1): 9-19. Fan Zhenhua, Li Xujun, Liang Bensheng, et al. Geochemical Characteristics and Tectonic Setting of Haigou Intrusion od Antu Jilin[J]. Global Geology, 2012, 31(1): 9-19.
[1] Ruan Dawei, Li Shunda, Bi Yaqiang, Liu Xingyu, Chen Xuhu, Wang Xingyuan, Wang Keyong. Ore-Controlling Structures and Deep Metallogenic Prediction of Aerhada Pb-Zn Deposit in Inner Mongolia [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(6): 1705-1716.
[2] Fu Junyu, Wang Yan, Zhong Hui, Song Weimin, Sun Wei, Na Fuchao, Qian Cheng, Yang Yajun, Pang Xuejiao, Jiang Shan. Geochemistry and Source Characteristics of Ultramafic Rocks in Tuquan Mangniuhai, Inner Mongolia [J]. Journal of Jilin University(Earth Science Edition), 2017, 47(4): 1172-1186.
[3] Wang Xi, Duan Mingxin, Ren Yunsheng, Hou Zhaoshuo, Sun Deyou, Hao Yujie. Characteristics of Fluid Inclusions and Mineralization Age of Badaguan Cu-Mo Deposit in Erguna Area, Inner Mongolia [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(5): 1354-1367.
[4] Sun Yuewu, Ding Haisheng, Liu Huan, Zhang Dejun, Gong Fanhao, Zheng Yuejuan. Fossil Plants from the Guadalupian Yujiabeigou Formation in the North Margin of North China Plate and Their Tectonic Implications [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(5): 1268-1283.
[5] Li Sanzhong, Yang Zhao, Zhao Shujuan, Li Xiyao, Suo Yanhui, Guo Lingli, Yu Shan, Dai Liming, Li Shaojun, Mu Dunling. Global Early Paleozoic Orogens (Ⅱ): Subduction-Accretionary-Type Orogeny [J]. Journal of Jilin University(Earth Science Edition), 2016, 46(4): 968-1004.
[6] Wang Chengyang, Wang Keyong, Zhou Xiangbin, Li Wen, Huang Guanghuan, Li Jianfeng, Zhang Xuebing, Yu Qi. Geochemical Characteristics of Ore-Forming Fluids and Genesis of Dongshanwan Tungsten- Molybdenum Polymetallic Deposit in Inner Mongolia [J]. Journal of Jilin University(Earth Science Edition), 2015, 45(3): 759-771.
[7] Han Jun, Xue Wei, Song Qingnian. Characteristics of Volcanic-Type Uranium-Ore Forming and Sign for Uranium Searching at Hetaoba Area, Duolun County, Inner Mongolia [J]. Journal of Jilin University(Earth Science Edition), 2015, 45(3): 772-790.
[8] Xi Aihua, Ma Yanjun, Ge Yuhui, Tang Xiangyang, Liu Shuai, Xu Bowen, Liu Jue. Multi-Stage Intrusive Evidence and Geological Significance of Dayingzi Granite in Chifeng,Eastern Inner Mongolia [J]. Journal of Jilin University(Earth Science Edition), 2015, 45(3): 791-803.
[9] Feng Xiaoxi, Yao Shuzhen, Duan Ming, Qu Kai, Wang Jiaying, Feng Xubiao, Li Chao, Zhou Limin. Re-Os Isotopic Dating of Molybdenite from the Bainaimiao Cu(Mo) Deposit in Inner Mongolia and Its Geological Significance [J]. Journal of Jilin University(Earth Science Edition), 2015, 45(1): 132-141.
[10] Wang Zhihua, Chang Chunjiao, Cong Runxiang, Wang Liang, Ma Dexi, Wang Xiaojun. SHRIMP Zircon U-Pb Age and Geochemical Characteristics of the Achieng Qulu Monzogranite in Inner Mongolia [J]. Journal of Jilin University(Earth Science Edition), 2015, 45(1): 166-187.
[11] LIU Yi-fei, NIE Feng-jun, JIANG Sai-hong, LIU Yan, LIANG Qing-ling. Bairendaba Pb-Zn-Ag Polymetallic Deposit in Inner Mongolia: The Mineralization Zoning and Its Origin [J]. J4, 2012, 42(4): 1055-1068.
[12] JIANG Si-hong, NIE Feng-jun, LIU Yi-fei, HOU Wan-rong, BAI Da-ming, LIU Yan, LIANG Qing-ling. Geochronology of Intrusive Rocks Occurring in and Around the Mengentaolegai Silver-Polymetallic Deposit, Inner Mongolia [J]. J4, 2011, 41(6): 1755-1769.
[13] BAI Da-ming, FU Guo-li, NIE Feng-jun, JIANG Si-hong, LIU Yi-fei. Integrated Ore-Prospecting Model for the Skarn Polymetallic Deposit in Southeastern Inner Mongolia [J]. J4, 2011, 41(6): 1968-1976.
[14] LI Jin-wen, LIANG Yu-wei, WANG Xiang-yang, ZHANG Bin, YANG Yun-cheng, SHE Hong-quan, GUO Zhi-jun. The Origin of the Erdaohezi Lead-Zinc Deposit, Inner Mongolia [J]. J4, 2011, 41(6): 1745-1754.
[15] LIU Yi-fei, NIE Feng-jun, JIANG Si-hong, XI Zhong, ZHANG Zhi-gang, XIAO Wei, ZHANG Ke, LIU Yong. Ore-Forming Fluid Characteristics and Ore Genesis of Chaganhua Porphyry Molybdenum Deposit in Central Inner Mongolia, China [J]. J4, 2011, 41(6): 1794-1805.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
Copyright © Journal of Jilin University(Earth Science Edition), All Rights Reserved.
Tel: +86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
Powered by Beijing Magtech Co. Ltd