LA-ICP-MS zircon U-Pb dating of the biotite monzonitic granite from Shihahe area in Inner Mongolia and its geological significance

HAO Zeng-yuan; NIU Yong-feng; CHEN Meng-chao; GAO Yong; CHEN Hai-dong; NIU Xue-ni

GEOLOGY IN CHINA > 2016 > 43(1): 72-80.

HAO Zeng-yuan, NIU Yong-feng, CHEN Meng-chao, GAO Yong, CHEN Hai-dong, NIU Xue-ni. LA-ICP-MS zircon U-Pb dating of the biotite monzonitic granite from Shihahe area in Inner Mongolia and its geological significance[J]. GEOLOGY IN CHINA, 2016, 43(1): 72-80.

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LA-ICP-MS zircon U-Pb dating of the biotite monzonitic granite from Shihahe area in Inner Mongolia and its geological significance

1. Inner Mongolia Institute of Geological Survey and Mineral Exploration, Hohhot 010010, Inner Mongolia, China;
2. Comprehensive Survey Party, Inner Mongolia Bureau of Nonferrous Geological Exploration, Hohhot 010010, Inner Mongolia, China;
3. Kunming University of Science and Technology, Kunming 650093 Yunnan, China

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Supported by China Geological Survey Program (No. 1212011120707).

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Received Date: December 25, 2014
Revised Date: March 03, 2015
Available Online: September 25, 2023

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Abstract

Abstract

Zircon U-Pb chronology and geochemistry of the biotite monzonitic granite from Shihahe area of Urad Middle Banner were studied systematically to investigate its formation age and tectonic background. The weighted average age obtained by zircon LA-ICP-MS U-Pb method is(274.99±0.71)Ma, which represents its formation age. The biotite monzonitic granite belongs to subaluminous-weakly peraluminous I-type and calc-alkaline series, with its A/CNK being 0.93-1.10 and σ being 2.01-2.88. The total REE (ΣREE) is lower, LREE values are higher and HREE is lower, with LREE/HREE ratio varying from 9.86 to 15.63, indicating that LREE and HREE differentiated intensely. Eu has insignificant anomalies or weakly negative anomalies. In the primitive mantle normalized trace elements spider diagram, the biotite monzogranite is enriched in large ion lithophile elements Rb and K while depleted in high field strength element Nb, similar to features of normal arc granitic rock. According to tectonic setting as well as emplacement time and characteristics of geochemistry of the biotite monzogranite from Shihahe area, it is inferred that the rocks were formed in an active continental margin environment, and the upper limit of conversion from ocean crust subduction to continent collision was later than late Early Permian.
- zircon U-Pb age,
- geochemistry,
- I-type granite,
- active continental margin,
- Urad Middle Banner

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References

[1]	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, 1991:351-352. Bureau of Geology and Mineral Resources of Inner Mongolia Autonomous Region. Regional geology of Inner Mongolia Autonomous Region[M]. Beijing:Geological Publish House, 1991:351-352(in Chinese).
[2]	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):824-836. 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):824-836(in Chinese with English abstract).
[3]	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, 2005:71-81. 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, 2005:71-86(in Chinese with English abstract).
[4]	张青伟, 刘正宏, 徐学纯, 等. 内蒙古乌拉特中期乌兰地区含石榴石花岗岩锆石U-Pb年龄及地质意义[J]. 吉林大学学报:地球科学版, 2011, 41(3):745-751. Zhang Qingwei, Liu Zhenghong, Xu Xuechun, et al. Zircon U-Pb dating of the garnet-bearing granite from Wulan area of Urad Zhongqi in Inner Mongolia and its geological significance[J]. Journal of Jilin University:Earth Science Edition, 2011, 41(3):745-751(in Chinese with English abstract).
[5]	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):1771-1780. Wang Wanqiong, Liu Zhenghong, Wang Xing'an, et al. SHRIMP U-Pb dating of the zircon from the Hercynian biotite monzonitic granites in Urad Zhongqi, Inner Mongolia, and its geological significance[J]. Journal of Jilin University:Earth Science Edition, 2012, 42(6):1771-1780(in Chinese with English abstract).
[6]	内蒙古自治区地质矿产局. 内蒙古自治区岩石地层[M]. 武汉:中国地质大学出版社, 1996:4-5. Bureau Geology and Mineral Resources of Inner Mongolia Autonomous Region. Lithostratic of Inner Mongolia Autonomous Region[M]. Wuhan:China University of Geosciences Press, 1996:4-5(in Chinese).
[7]	李怀坤, 耿建珍, 郝爽, 等. 用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究[J]. 矿物学报, 2009, 29(增刊):600-601. Li Huaikun, Geng Jianzhen, Hao Shuang, et al. Research on the dating zircon U-Pb age by LA-MC-ICPMS[J]. Journal of Mineralogy, 2009, 29(Sup.):600-601(in Chinese with English abstract).
[8]	Ludwig K R. Squid 1.02:A user's manual[J]. Berkeley Geochronology Centre, Special Publication, 2001(2):15-25.
[9]	吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 2004, 46(16):1589-1604. Wu Yuanbao, Zheng Yongfei. Genetic mineralogy of zircons and its constraints to the age of U-Pb geochronology[J]. Chinese Science Bulletin, 2004, 46(16):1589-1604(in Chinese with English abstract).
[10]	李志昌, 路远发, 黄圭成. 放射性同位素地质学方法与进展[M]. 武汉:中国地质大学出版社, 2004:160-164. Liu Zhichang, Lu Yuanfa, Huang Guicheng. Methodology and Progress in Radioactivity Isotope Geology[M]. Wuhan:China University of Geosciences Press, 2004:160-164(in Chinese).
[11]	桑隆康, 马昌前. 岩石学[M]. 北京:地质出版社, 2012:72-78, 181-197. Shang Longkang, Ma Changqian. Petrology[M]. Beijing:Geological Publishing House, 2012:72-78, 181-197(in Chinese).
[12]	柏道远, 陈必河, 孟德保, 等. 中昆仑耸石山地区万古时代花岗岩地球化学特征、成岩作用与构造环境研究[J]. 中国地质, 2006, 33(6):1236-1245. Bai Daoyuan, Chen Bihe, Meng Debao, et al.Geochemical characteristics, rock forming processes and tectonic setting of Later Paleozoic granites in the Songshishan area, Central Kunlun mountains[J]. Geology in China, 2006, 33(6):1236-1245(in Chinese with English abstract).
[13]	Hugh R.Rollison. 岩石地球化学[M]. 杨学明, 杨晓勇, 陈双喜, 译. 合肥:中国科学技术大学出版社, 2000:106-117, 155-157. Rollison H R. Petrological Geochemistry[M]. Yang Xueming, Yang Xiaoyong, Chen Shuangxi(translators). Hefei:Press of University of Science and Technology of China, 2000:106-117, 155-157(in Chinese).
[14]	赵庆英, 刘正宏, 吴新伟, 等. 内蒙古大青山哈拉和少岩体特征和成因[J]. 岩石矿物, 2007, 27(1):46-51. Zhao Qingying, Liu Zhenghong, Wu Xinwei, et al. Characteristics and origin of Haleheshao pluton in Daqingshan region, Inner Mongolia[J]. Journal of Mineralogy and Petrology, 2007, 27(1):46-51(in Chinese with English abstract).
[15]	赵振华. 关于岩石微量元素构造环境判别图解使用的有关问题[J]. 大地构造与成矿学, 2007, 31(1):92-103. Zhao Zhenhua. How to use the trace element diagrams to discriminate tectonic setting[J]. Geotectonica et Metallogenia, 2007, 31(1):92-103(in Chinese with English abstract).
[16]	邵济安, 唐克东. 蛇绿岩与蒙古洋的演化[C]//张旗主编. 蛇绿岩与地球动力学研究. 北京:地质出版社, 1996:117-119. Shao Ji'an, Tang Kedong. Ophiolite and the evolution of Mongolia Ocean[C]//Zhang Qi (ed.). Study on Ophiolites and Geodynamics. Beijing:Geological Publishing House, 1996:117-119(in Chinese with English abstract).
[17]	赵磊, 吴泰然, 罗红玲. 内蒙古乌拉特中旗北七哥陶辉长岩SHRIMP锆石U-Pb年龄、地球化学特征及其地质意义[J]. 岩石学报, 2011, 27(10):3071-3082. Zhao Lei, Wu Tairan, Luo Hongling. SHRIMP U-Pb dating, geochemistry and tectonic implications of Beiqigetao gabbors in Urad Zhongqi area, Inner Mongolia[J]. 2011, 27(10):3071-3082(in Chinese with English abstract).
[18]	陶继雄, 白立斌, 宝音乌力吉, 等. 内蒙古满都拉地区二叠纪俯冲造山过程的岩石记录[J]. 地质调查与研究, 2003, 26(4):241-249. Tao Jixiong, Bai Libing, Bao Yinwuliji, et al. Rock record of Permian subducting orogenic process in Mandula, Innermongolia[J]. Geological Survey and Research, 2003, 26(4):241-249(in Chinese with English abstract).
[19]	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, 2010:71-86. Liu Changfeng. Paleozoic-Early Mesozoic magmatic belts tectonic significance in Siziwangqi area, Inner Mongolia[D]. Beijing:China University of Geosciences, 2010:71-86(in Chinese with English abstract).
[20]	陆凤香, 桑隆康. 岩石学[M]. 北京:地质出版社, 2002:373-380. Lu Fengxiang, Sang Longkang. Petrology[M]. Beijing:Geological Publishing House, 2002:373-380(in Chinese).

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LA-ICP-MS zircon U-Pb dating of the biotite monzonitic granite from Shihahe area in Inner Mongolia and its geological significance

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