Detrital zircon U-Pb age of siltstone from Linxi Formation in Balinyouqi, Inner Mongolia : constraints on the final closure of the Paleo-Asian Ocean

ZHANG Shengxu; CHEN Fengjie; DING Jishuang; ZHAO Chao; YANG Wenpeng; YANG Fushen

doi:10.12097/j.issn.1671-2552.2022.10.006

2022 Vol. 41, No. 10

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ZHANG Shengxu, CHEN Fengjie, DING Jishuang, ZHAO Chao, YANG Wenpeng, YANG Fushen. Detrital zircon U-Pb age of siltstone from Linxi Formation in Balinyouqi, Inner Mongolia : constraints on the final closure of the Paleo-Asian Ocean[J]. Geological Bulletin of China, 2022, 41(10): 1757-1771. doi: 10.12097/j.issn.1671-2552.2022.10.006

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ZHANG Shengxu, CHEN Fengjie, DING Jishuang, ZHAO Chao, YANG Wenpeng, YANG Fushen. Detrital zircon U-Pb age of siltstone from Linxi Formation in Balinyouqi, Inner Mongolia : constraints on the final closure of the Paleo-Asian Ocean[J]. Geological Bulletin of China, 2022, 41(10): 1757-1771. doi: 10.12097/j.issn.1671-2552.2022.10.006

Detrital zircon U-Pb age of siltstone from Linxi Formation in Balinyouqi, Inner Mongolia : constraints on the final closure of the Paleo-Asian Ocean

1.
Heilongjiang Natural Resources Investigation Institute, Harbin 150036, Heilongjiang, China
2.
Department of Geological and Surveying Engineering, Shanxi Institute of Energy, Jinzhong 030600, Shanxi, China

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Corresponding author: CHEN Fengjie, chen_fengjie0516@163.com

Received Date: 22 December 2020

Revised Date: 16 October 2021

Publish Date: 15 October 2022

Abstract

Abstract

In this paper, detrital zircon U-Pb ages were studied with the aims to reveal the formation ages and associated tectonic settings of clastic rocks from Linxi Formation in the north Xilamulun River, Balinyouqi, Inner Mongolia.The LA-ICP-MS results show that the 98 zircons grains show concordant ages of 252~315 Ma, 376~523 Ma, 752~1097 Ma, 1465~1694 Ma and 1833~2563 Ma.The youngest zircons age is 252 Ma, which indicates that the lower sedimentary age of the Linxi Formation is the Late Permian.The zircon age spectrum map, which includes the age information of both the southern margin of the Central Asian Orogenic Belt (CAOB) and northern margin of the North China Craton (NCC), showt that the stratum was characterized by multi-sources.This indicates that the materials in the Linxi Formation was mainly sourced from the south margin of the CAOB with minor from the northern margin of the NCC.The sample age information and the previous Paleontological stratigraphy and Paleomagnetic studies indicate that the sedimentary time of the Linxi Formation is the late Middle Permian to early Early Triassic, with the main sedimentary time of Late Permian.Combined with the comparison of regional strata and tectonic evolution in the eastern CAOB, the authors conclude that the Paleo Asian Ocean was likely final closed during the Late Permian.
- Balinyouqi /
- Linxi Formation /
- siltstone /
- detrital zircon /
- LA-ICP-MS U-Pb age /
- geological survey engineering /
- Inner Mongolia

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References

[1]	曹从周, 杨芳林, 田昌裂, 等. 内蒙古贺根山地区蛇绿岩及中朝板块和西伯利亚板块之间的缝合带位置[C]//中国北方板块构造论文集. 北京: 地质出版社, 1986: 64-86. Google Scholar
[2]	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与演化[J]. 中国科学, 1997, 27(3): 227-232. Google Scholar
[3]	Robinson P T, Zhou M F, Hu X F, et al. Geochemical constraints on the origin of the Hegenshan ophiolite, Inner Mongolia, China[J]. Journal of Asian Earth Sciences, 1999, 17(4): 423-442. doi: 10.1016/S1367-9120(99)00016-4 CrossRef Google Scholar
[4]	Nozaka T, Liu Y. Petrology of the Hegenshan ophiolite and its implication for the tectonic evolution of northern China[J]. Earth and Planetary Science Letters, 2002, 202(202): 89-104. Google Scholar
[5]	李春昱, 王荃. 我国北部边陲及邻区的古板块构造与欧亚大陆的形成. [C]//中国北方板块构造文集. 北京: 地质出版社, 1983: 3-16. Google Scholar
[6]	Wu F Y, Sun D Y, Li H M, et al. A-type granites in northeastern china; Age and geochemical constraints on their petrogenesis[J]. Chemical Geology, 2002, 187: 143-173. doi: 10.1016/S0009-2541(02)00018-9 CrossRef Google Scholar
[7]	Wu F Y, Wilde S A, Zhang G L, et al. Geochronology and petrogenesis of the post-orogentic Cu Ni ulfide-bearing mafic ultramafic completes in Jilin Province, NE China[J]. Journal of Asian Earth Sci., 2004, 23: 781-797. doi: 10.1016/S1367-9120(03)00114-7 CrossRef Google Scholar
[8]	尚庆华. 北方造山带内蒙古中东部地区二叠纪放射虫的发现及意义[J]. 科学通报, 2004, 49(34): 2574-2579. Google Scholar
[9]	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, 2004, 34(2): 174-180. Google Scholar
[10]	李锦轶, 高立明, 孙桂华, 等. 内蒙古东部双井子中三叠世同碰撞壳源花岗岩及其对西伯利亚与中朝古板块碰撞时限的约束[J]. 岩石学报, 2007, 23(3): 565-582. Google Scholar
[11]	谭晓淼, 高锐, 王海燕, 等. 中亚造山带东段深地震反射剖面大炮揭露下地壳与Moho结构——数据处理与初步解释[J]. 吉林大学学报(地球科学版), 2021, 51(3): 898-908. Google Scholar
[12]	谢樊, 王海燕, 侯贺晟, 等. 中亚造山带东段浅表构造速度结构——深地震反射剖面初至波层析成像的揭露[J]. 吉林大学学报(地球科学版), 2021, 51(2): 584-596. Google Scholar
[13]	张健, 张德军, 郑月娟, 等. 内蒙古林西上二叠统林西组碎屑锆石LA-ICP-MS年代学及其构造意义[J]. 吉林大学学报(地球科学版), 2020, 50(4): 1090-1103. Google Scholar
[14]	杜继宇, 陶楠, 郭建超, 等. 内蒙古巴林右旗巴彦查干岩体年代学与地球化学: 对古亚洲洋闭合时间的限定[J]. 地球科学, 2019, 44(10): 3361-3377. Google Scholar
[15]	郑月娟, 张海华, 陈树旺, 等. 内蒙古阿鲁科尔沁旗林西组碎屑锆石LA-ICP-MS U-Pb测年及意义[J]. 地质通报, 2014, 33(9): 1293-1307. doi: 10.3969/j.issn.1671-2552.2014.09.004 CrossRef Google Scholar
[16]	王金芳, 李英杰, 李红阳, 等. 古亚洲洋俯冲板片断离与后造山伸展: 贺根山缝合带火山岩年代学和地球化学证据[J]. 地质学报, 2020, 94(12): 3561-3580. doi: 10.3969/j.issn.0001-5717.2020.12.004 CrossRef Google Scholar
[17]	韩国卿, 刘永江, 温泉波, 等. 西拉木伦河缝合带北侧二叠纪砂岩碎屑锆石LA-ICP-MS U-Pb年代学及其构造意义[J]. 地球科学(中国地质大学学报), 2011, 36(4): 687-702. Google Scholar
[18]	王必任. 内蒙古罕乌拉地区晚石炭世—早二叠世火山—沉积地层及其构造变形——对中亚造山带东南段索伦缝合带构造演化的启示[D]. 中国地震局地质研究所博士学位论文, 2020. Google Scholar
[19]	韩杰, 周建波, 张兴洲, 等. 内蒙古林西地区上二叠统林西组砂岩碎屑锆石的年龄及其大地构造意义[J]. 地质通报, 2011, 31(2): 258-269. doi: 10.3969/j.issn.1671-2552.2011.02.011 CrossRef Google Scholar
[20]	黄本宏. 内蒙古东部陶海营子组植物化石[J]. 植物学报, 1983, (6): 580-583. Google Scholar
[21]	王成源, 王平, 李文国. 内蒙古二叠系哲斯组的牙形刺及其时代[J]. 古生物学报, 2006, 45(2): 195-206. doi: 10.3969/j.issn.0001-6616.2006.02.004 CrossRef Google Scholar
[22]	郑月娟, 公繁浩, 陈树旺, 等. 内蒙古西乌珠穆沁旗地区下二叠统原寿山沟组碎屑锆石LA-ICP-MS U-Pb年龄及地质意义[J]. 地质通报, 2013, 32(8): 1260-1268. doi: 10.3969/j.issn.1671-2552.2013.08.012 CrossRef Google Scholar
[23]	赵英利. 大兴安岭中南部二叠纪砂岩物源分析对晚古生代区域构造演化的制约[D]. 吉林大学博士学位论文, 2010. Google Scholar
[24]	徐增连, 骆满生, 杨文麟, 等. 额尔齐斯-西拉木伦对接带古生代沉积盆地演化[J]. 地球科学——中国地质大学学报, 2014, (8): 1099-1118. Google Scholar
[25]	王友勤, 苏养正. 武汉: 中国东北岩石地层[M]. 武汉: 中国地质大学出版社, 1996: 219-220. Google Scholar
[26]	程三友, 刘少峰, 苏三. 索伦-林西缝合带北侧西段中二叠统哲斯组砂岩碎屑分析及其构造意义[J]. 东华理工大学学报: 自然科学版, 2013, 36(2): 161-167. doi: 10.3969/j.issn.1674-3504.2013.02.009 CrossRef Google Scholar
[27]	金玉玕. 中国地层典[M]. 北京: 地质出版社, 2000. Google Scholar
[28]	方曙, 张忠, 于海洋, 等. 内蒙古东部大地构造[M]. 北京: 地质出版社, 2013. Google Scholar
[29]	Belousova E, Griffin W, O'Reilly S Y, et al. Igneous zircon: trace element composition as an indicator of source rock type[J]. Contributions to Mineralogy & Petrology, 2002, 143(5): 602-622. Google Scholar
[30]	李文国. 内蒙古自治区岩石地层[M]. 武汉: 中国地质大学出版社, 1996. Google Scholar
[31]	Fedo C M. Detrital zircon analysis of the sedimentary record[J]. Reviews in Mineralogy & Geochemistry, 2003, 53(1): 277-303. Google Scholar
[32]	Griffin W L, Belousova E A, Shee S R, et al. Archean crustal evolution in the northern Yilgarn Craton: U-Pb and Hf-isotope evidence from detrital zircons[J]. Precambrian Research, 2004, 131(3): 231-282. Google Scholar
[33]	李雨柯. 内蒙古东部索伦二叠纪哲斯组碎屑锆石U-Pb年龄及其大地构造意义[J]. 科学技术与工程, 2012, 20(25): 6269-6277. doi: 10.3969/j.issn.1671-1815.2012.25.004 CrossRef Google Scholar
[34]	宋卫卫, 周建波, 郭晓丹, 等. 松辽地块大地构造属性: 古生界碎屑锆石年代学的制约[J]. 世界地质, 2012, 31(3): 522-535. doi: 10.3969/j.issn.1004-5589.2012.03.009 CrossRef Google Scholar
[35]	刘建峰, 李锦轶, 孙立新, 等. 内蒙古巴林左旗九井子蛇绿岩锆石U-Pb定年: 对西拉木伦河缝合带形成演化的约束[J]. 中国地质, 2016, 43(6): 1947-1962. Google Scholar
[36]	李红英, 张达, 周志广, 等. 内蒙古克什克腾旗林西组碎屑锆石LA-ICP-MS年代学及其地质意义[J]. 吉林大学学报(地球科学版), 2016, 46(1): 146-162. Google Scholar
[37]	李晓海, 宗文明, 苏飞, 等. 内蒙古扎鲁特旗上二叠统林西组碎屑锆石LA-ICP-MSU-Pb测年及意义[J]. 地质与资源, 2015, 24(5): 461-472. doi: 10.3969/j.issn.1671-1947.2015.05.011 CrossRef Google Scholar
[38]	张海华, 郑月娟, 陈树旺, 等. 内蒙古巴林左旗二叠系碎屑锆石LA-ICP-MS U-Pb年龄及构造意义[J]. 地质学报, 2015, 89(10): 1703-1717. doi: 10.3969/j.issn.0001-5717.2015.10.001 CrossRef Google Scholar
[39]	高德臻, 蒋干清. 内蒙古苏尼特左旗二叠系的重新厘定及大地构造演化分析[J]. 地质通报, 1998, 17(4): 401-411. Google Scholar
[40]	雷豪, 张贵宾, 徐备. 兴蒙造山带晚古生代伸展减薄过程: 来自内蒙林西地区岩体的地球化学证据[J]. 岩石学报, 2021, 37(7): 2029-2050. Google Scholar
[41]	杨文鹏, 张生旭, 姜海洋, 等. 内蒙古巴林右旗晚二叠世埃达克质火山岩特征及其地质意义[J]. 地质通报, 2018, 37(9): 1710-1721. Google Scholar
[42]	李益龙, 周汉文, 钟增球, 等. 华北与西伯利亚板块的对接过程: 来自西拉木伦缝合带变形花岗岩锆石LA-ICP-MS U-Pb年龄证据[J]. 地球科学——中国地质大学学报, 2009, 34(6): 931-938. Google Scholar
[43]	章永梅, 张华锋, 刘文灿, 等. 内蒙古中部四子王旗大庙岩体时代及成因[J]. 岩石学报, 2009, 25(12): 3165-3181. Google Scholar
[44]	范宏瑞, 胡芳芳, 杨奎锋, 等. 内蒙古白云鄂博地区晚古生代闪长质-花岗质岩石年代学框架及其地质意义[J]. 岩石学报, 2009, 25(11): 2933-2938. Google Scholar
[45]	鲁颖淮, 李文博, 赖勇. 内蒙古镶黄旗哈达庙金矿床含矿斑岩体形成时代和成矿构造背景[J]. 岩石学报, 2009, 25(10): 2615-2620. Google Scholar
[46]	王芳, 陈福坤, 侯振辉, 等. 华北陆块北缘崇礼—赤城地区晚古生代花岗岩类的锆石年龄和Sr-Nd-Hf同位素组成[J]. 岩石学报, 2009, (11): 3057-3074. Google Scholar
[47]	张永生, 牛绍武, 田树刚, 等. 内蒙古林西地区上二叠统林西组叶肢介化石的发现及意义[J]. 地质通报, 2012, 31(9): 1394-1403. Google Scholar
[48]	邓胜徽, 万传彪, 杨建国. 黑龙江阿城晚二叠世安加拉-华夏混生植物群——兼述古亚洲洋的关闭问题[J]. 中国科学, 2009, (12): 1744-1752. Google Scholar
[49]	李朋武, 高锐, 管烨, 等. 内蒙古中部索伦林西缝合带封闭时代的古地磁分析[J]. 吉林大学学报(地球科学版), 2006, 36(5): 744-758. Google Scholar
[50]	秦华峰, 李永飞, 黄晟, 等. 内蒙古阿鲁科尔沁旗二叠纪地层古地磁研究结果及其构造意义[J]. 地质通报, 2013, 32(2): 388-398. Google Scholar
[51]	刘敦一, 简平, 张旗, 等. 内蒙古图林凯蛇绿岩中埃达克岩SHRIMP测年: 早古生代洋壳消减的证据[J]. 地质学报, 2003, 77(3): 318-327. Google Scholar
[52]	Ping J, Liu D, Kr Ner A, et al. Time scale of an early to mid-Paleozoic orogenic cycle of the long-lived Central Asian Orogenic Belt, Inner Mongolia of China: Implications for continental growth[J]. Lithos, 2008, 101(3/4): 233-259. Google Scholar
[53]	Miao L C, Zhang F Q, Fan W M, et al. Phanerozoic evolution of the Inner Mongolia Daxinganling orogenic belt in North China: constraints from geochronology of ophiolites and associated formations[J]. Geological Society London Special Publications, 2007, 280(1): 223-237. Google Scholar
[54]	石玉若, 刘敦一, 张旗, 等. 内蒙古苏左旗地区闪长-花岗岩类SHRIMP年代学[J]. 地质学报, 2004, 78(6): 789-789. Google Scholar
[55]	薛怀民, 郭利军, 侯增谦, 等. 中亚-蒙古造山带东段的锡林郭勒杂岩: 早华力西期造山作用的产物而非古老陆块?——锆石SHRIMP U-Pb年代学证据[J]. 岩石学报, 2009, 25(8): 2001-2010. Google Scholar
[56]	孙立新, 任邦方, 赵凤清, 等. 内蒙古锡林浩特地块中元古代花岗片麻岩的锆石U-Pb年龄和Hf同位素特征[J]. 地质通报, 2013, 32(2): 327-340. Google Scholar
[57]	孙立新, 赵凤清, 王惠初, 等. 内蒙古狼山地区宝音图地块变质基底的锆石U-Pb年龄及构造意义[J]. 地质学报, 2013, 87(2): 197-207. Google Scholar
[58]	裴福萍, 许文良, 杨德彬, 等. 松辽盆地基底变质岩中锆石U-Pb年代学及其地质意义[J]. 科学通报, 2006, (24)): 2881-2887. Google Scholar
[59]	Wilde S A, Zhang X, Wu F. Extension of a newly identified 500 Ma metamorphic terrane in North East China: further U-Pb SHRIMP dating of the Mashan Complex, Heilongjiang Province, China[J]. Tectonophysics, 2000, 328(1): 115-130. Google Scholar
[60]	Wilde S A, F Wu, Zhang X. Late Pan-African magmatism in northeastern China: SHRIMP U-Pb zircon evidence from granitoids in the Jiamusi Massif[J]. Precambrian Research, 2003, 122(1): 311-327. Google Scholar
[61]	赵院冬, 许逢明, 车继英, 等. 锆石U-Pb定年对大兴安岭东北部"兴华渡口群"形成时代和组成的约束[J]. 中国地质, 2017, 44(3): 575-587. Google Scholar
[62]	施光海, 刘敦一, 张福勤, 等. 中国内蒙古锡林郭勒杂岩SHRIMP锆石U-Pb年代学及意义[J]. 科学通报, 2003.48(20): 2187-2192. Google Scholar
[63]	郭晓丹, 周建波, 张兴洲, 等. 内蒙古西乌珠穆沁旗本巴图组碎屑锆石LA-ICP-MS U-Pb年龄及其意义[J]. 地质通报, 2011, 31(2): 278-290. Google Scholar
[64]	宋卫卫, 周建波, 郭晓丹, 等. 松辽地块大地构造属性: 古生界碎屑锆石年代学的制约[J]. 世界地质, 2012, 31(3): 522-535. Google Scholar
[65]	章凤奇, 陈汉林, 董传万, 等. 松辽盆地北部存在前寒武纪基底的证据[J]. 中国地质, 2008, 35(3): 421-428. Google Scholar
[66]	葛文春, 隋振民, 吴福元, 等. 大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及地质意义[J]. 岩石学报, 2007, 23(2): 423-440. Google Scholar
[67]	翟明国, 胡波, 彭澎, 等. 华北中—新元古代的岩浆作用与多期裂谷事件[J]. 地学前缘, 2014, 21(1): 100-119. Google Scholar
[68]	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. Google Scholar
[69]	Guan H, Sun M, Wilde S A, et al. SHRIMP U-Pb zircon geochronology of the Fuping Complex: implications for formation and assembly of the North China Craton[J]. Precambrian Research, 2002, 113(1/2): 1-18. Google Scholar
[70]	翟明国. 华北克拉通的形成以及早期板块构造[J]. 地质学报, 2012, 86(9): 1335-1349. Google Scholar
[71]	周建波, 张兴洲, Simon A WILDE, 等. 中国东北~500 Ma泛非期孔兹岩带的确定及其意义[J]. 岩石学报, 2011, 27(4): 1235-1245. Google Scholar
[72]	权京玉, 迟效国, 张蕊, 等. 松嫩地块东部新元古代东风山群碎屑锆石LA-ICP-MS U-Pb年龄及其地质意义[J]. 地质通报, 2013, 32(2/3): 353-364. Google Scholar
[73]	尚庆华. 北方造山带内蒙古中东部地区二叠纪放射虫的发现及意义[J]. 科学通报, 2004, 49(24): 2574-2579. Google Scholar
[74]	程招勋, 汪岩, 钱程, 等. 内蒙古乌兰浩特古元古代变质岩系的发现及其地质意义[J]. 地质通报, 2018, 37(9): 1599-1606. Google Scholar
[75]	张超, 吴新伟, 刘正宏, 等. 松嫩地块西缘前寒武岩浆事件——来自龙江地区古元古代花岗岩锆石LA-ICP-MS U-Pb年代学证据[J]. 岩石学报, 2017, 34(10): 3137-3152. Google Scholar
[76]	吴迪迪, 李舢, David Chew, 等. 中亚造山带东南缘二叠纪-三叠纪花岗质岩浆演化对增生-碰撞过程的制约[J]. 中国科学: 地球科学, 2021, 51(6): 906-926. Google Scholar