华北板块北缘东段库伦杂岩的发现及其构造意义

doi:10.13686/j.cnki.dzyzy.2024.01.001

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Abstract The Kulun complex, mainly composed of Late Paleozoic meta-volcanic rocks, has been newly discovered in Kulun Qi area on the border between Liaoning and Inner Mongolia in the east part of the northern margin of North China Plate. The profile survey confirms the rock association of Kulun complex including tuff, andesite and metasedimentary rock. The zircon LA-ICP-MS U-Pb isotope test for the tuff shows 391.0±3.7 Ma, indicating the formation age of Middle Devonian. The geochemical characteristics show that the complex was formed in later island arc environment. The tectonic evolution process of the Paleozoic accretionary orogenic belt in the east part of the northern margin of North China Plate is established through the study of the newly discovered Middle Devonian Kulun complex and related Paleozoic sedimentary events, magmatic events and deformation, combined with the research results of the Paleozoic complex, magmatic rocks and volcanic sedimentary strata in the area. The orogenic belt has experienced the Silurian active continental margin stage, Devonian arc-continental collision stage, Carboniferous-Middle Permian active continental margin stage and Late Permian collision orogenic stage. The Silurian Fangjiatun and Xibiehe rock formations were formed in the back-arc basin environment, indicating the study area was in the active continental margin environment during the Ordovician-Silurian. The volcano-sedimentation of the Devonian Kulun complex is the result of arc-continent collision, accompanied by magmatic activity under extensional background. The study area underwent pull-apart again under the post-collision extension background, and received the deposits of Baijiadian rock formation and Jiujuzi rock formation in the Carboniferous-Middle Permian, leading to the formation of the volcanic island arc of Tongjiatun rock formation. In the Late Permian, continent-continent collision occurred with the closure of Paleo-Asian Ocean, and the post-orogeny continued to the Triassic.

Key words： Kulun complex accretionary orogenic belt Xing'an-Mongolian orogenic belt North China Plate Paleozoic tectonic evolution

Received: 17 July 2022

PACS:	P597
	P544

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	LI Dong-tao
	LIU Jin
	CHEN Jing-sheng
	ZHAO Chen
	LI Yu-chao
	PENG You-bo
	KUAI Bing
	YANG Zhong-jie
	LIU Wen-bin

Cite this article:

LI Dong-tao,LIU Jin,CHEN Jing-sheng等. DISCOVERY OF KULUN COMPLEX IN THE EAST PART OF THE NORTHERN MARGIN OF NORTH CHINA PLATE:Tectonic Implication[J]. GEOLOGY AND RESOURCES, 2024, 33(1): 1-11,40.

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http://manu25.magtech.com.cn/Jweb_dzyzy/EN/10.13686/j.cnki.dzyzy.2024.01.001 OR http://manu25.magtech.com.cn/Jweb_dzyzy/EN/Y2024/V33/I1/1

[1]	谢鸣谦. 拼贴板块构造及其驱动机理——中国东北及邻区的大地构造演化[M]. 北京:科学出版社, 2000:1-256. Xie M Q. Collage plate tectonics and its driving mechanism:Tectonic evolution of Northeast China and its adjacent areas[M]. Beijing: Science Press, 2000:1-256. (in Chinese)
[2]	唐克东, 鞠楠, 张大权, 等. 关于古亚洲洋构造演化研究的几点思考[J]. 地质与资源, 2022, 31(3):246-258,330. Tang K D, Ju N, Zhang D Q, et al. Implication of the tectonic evolution of Paleo-Asian Ocean[J]. Geology and Resources, 2022, 31(3):246-258,330.
[3]	时溢, 石绍山, 舒广龙. 辽宁北部早古生代弧-陆碰撞作用的发现及其构造意义[J]. 地质与资源, 2020, 29(4):397-400. Shi Y, Shi S S, Shu G L. Discovery of the Early Paleozoic arc-continent collision in northern Liaoning Province:Tectonic implication[J]. Geology and Resources, 2020, 29(4):397-400.
[4]	周建波, 张兴洲, 马志红, 等. 中国东北地区的构造格局与盆地演化[J]. 石油与天然气地质, 2009, 30(5):530-538. Zhou J B, Zhang X Z, Ma Z H, et al. Tectonic framework and basin evolution in Northeast China[J]. Oil & Gas Geology, 2009, 30(5): 530-538.
[5]	刘永江, 张兴洲, 金巍, 等. 东北地区晚古生代区域构造演化[J]. 中国地质, 2010, 37(4):943-951. Liu Y J, Zhang X Z, Jin W, et al. Late Paleozoic tectonic evolution in Northeast China[J]. Geology in China, 2010, 37(4):943-951.
[6]	王成文, 金巍, 张兴洲, 等. 东北及邻区晚古生代大地构造属性新认识[J]. 地层学杂志, 2008, 32(2):119-136. Wang C W, Jin W, Zhang X Z, et al. New understanding of the Late Paleozoic tectonics in northeastern China and adjacent areas[J]. Journal of Stratigraphy, 2008, 32(2):119-136.
[7]	李双林, 欧阳自远. 兴蒙造山带及邻区的构造格局与构造演化[J]. 海洋地质与第四纪地质, 1998, 18(3):45-54. Li S L, Ouyang Z Y. Tectonic framework and evolution of Xing'anling-Mongolian Orogenic Belt (XMOB) and its adjacent region[J]. Marine Geology & Quaternary Geology, 1998, 18(3):45-54.
[8]	李继亮. 增生型造山带的基本特征[J]. 地质通报, 2004, 23(9/10): 947-951. Li J L. Basic characteristics of accretion-type orogens[J]. Geological Bulletin of China, 2004,23(9/10):947-951.
[9]	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 B, Chen B. The structure and evolution of the Mesozoic orogenic belt between the North China Plate and the Siberian Plate in northern Inner Mongolia[J]. Science in China (Series D), 1997, 27(3):227- 232. (in Chinese)
[10]	Roser B P, Korsch R J. Determination of tectonic setting of sandstone-mudstone suites using silica content and potassium oxide/ sodium oxide ratio[J]. The Journal of Geology, 1986, 94(5):635-650.
[11]	Bhatia M R. Plate tectonics and geochemical composition of sandstones[J]. The Journal of Geology, 1983, 91(6):611-627.
[12]	Pearce J A, Harris N B W, Tindle A G. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 1984, 25:956-983.
[13]	Condie K C. Geochemistry and tectonic setting of Early Proterozoic supracrustal rocks in the southwestern United States[J]. The Journal of Geology, 1986, 94(6):845-864.
[14]	杨泽黎,刘洋,滕飞,等. 白乃庙岛弧东段早古生代火山岩年代学、地球化学特征及地质意义[J]. 高校地质学报, 2019,25(2):206- 220. Yang Z L, Liu Y, Teng F, et al. Geochronology and geochemistry of the Early Paleozoic volcanic rocks in eastern segment of the Bainaimiao arc, and their geological significances[J]. Geological Journal of China Universities, 2019,25(2):206-220.
[15]	胡晓佳,杨泽黎,王树庆,等. 内蒙古包尔汉图岛弧早古生代火山岩年代学、地球化学特征——岩石成因及对兴蒙造山带构造演化的约束[J]. 地质学报,2022,96(3):897-917. Hu X J, Yang L Z, Wang S Q, et al. Geochronology and geochemistry of the Early Paleozoic volcanic rocks from the Baoerhantu arc in Inner Mongolia:Petrogenesis and constraints on the tectonic evolution of the Xing-Meng orogenic belt[J]. Acta Geologica Sinica, 2022,96(3):897-917.
[16]	Shi Y, Shi S S, Liu Z H, et al. Petrogenesis of the late Early Palaeozoic adakitic granitoids in the southern margin of the Songliao Basin, NE China:Implications for the subduction of the Palaeo-Asian Ocean[J]. Geological Journal, 2019, 54(6):3821-3839.
[17]	李锦轶,张进,杨天南,等. 北亚造山区南部及其毗邻地区地壳构造分区与构造演化[J]. 吉林大学学报(地球科学版), 2009,39(4): 584-605. Li J Y, Zhang J, Yang T N, et al. Crustal tectonic division and evolution of the southern part of the North Asian Orogenic region and its adjacent areas[J]. Journal of Jilin University (Earth Science Edition), 2009,39(4):584-605.
[18]	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 S H, Zhao Y, Liu J M, 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.
[19]	罗镇宽,苗来成,关康,等. 河北张家口水泉沟岩体SHRIMP年代学研究及其意义[J]. 地球化学, 2001,30(2):116-122. Luo Z K, Miao L C, Guang K, et al. SHRIMP chronological study of Shuiquangou intrusive body in Zhangjiakou area, Hebei Province and its geochemical significance[J]. Geochimica, 2001,30(2):116-122.
[20]	刘建峰,李锦轶,迟效国,等. 华北克拉通北缘与弧-陆碰撞相关的早泥盆世长英质火山岩——锆石U-Pb定年及地球化学证据[J]. 地质通报, 2013,32(2/3):267-278. Liu J F, Li J Y, Chi X G, et al. Early Devonian felsic volcanic rocks related to the arc-continent collision on the northern margin of North China craton:Evidences of zircon U-Pb dating and geochemical characteristics[J]. Geological Bulletin of China, 2013,32(2/3):267- 278.
[21]	Liu J M, Zhao Y, Sun Y L, et al. Recognition of the latest Permian to Early Triassic Cu-Mo mineralization on the northern margin of the North China block and its geological significance[J]. Gondwana Research, 2010,17(1):125-134.
[22]	Shi Y R, Liu D Y, Miao L C, et al. Devonian A-type granitic magmatism on the northern margin of the North China Craton:SHRIMP U-Pb zircon dating and Hf-isotopes of the Hongshan granite at Chifeng, Inner Mongolia, China[J]. Gondwana Research, 2010,17(4):632-641.
[23]	Zhang S H, Zhao Y, Song B, et al. Petrogenesis of the Middle Devonian Gushan diorite pluton on the northern margin of the North China block and its tectonic implications[J]. Geological Magazine, 2007,144(3):553-568.
[24]	王惠初,赵凤清,李惠民,等. 冀北闪长质岩石的锆石SHRIMP U-Pb年龄:晚古生代岩浆弧的地质记录[J].岩石学报, 2007,23(3): 597-604. Wang H C, Zhao F Q, Li H M, et al. Zircon SHRIMP U-Pb age of the dioritic rocks from northern Hebei:The geological records of Late Paleozoic magmatic arc[J]. Acta Petrologica Sinica, 2007,23(3): 597-604.
[25]	张拴宏,赵越,宋彪,等. 冀北隆化早前寒武纪高级变质区内的晚古生代片麻状花岗闪长岩-锆石SHRIMP U-Pb年龄及其构造意义[J]. 岩石学报, 2004,20(3):621-626. Zhang S H, Zhao Y, Song B, et al. The Late Paleozoic gneissic granodiorite pluton in Early Pre-Cambrian high-grade metamorphic terrains near Longhua County in northern Hebei Province, North China:Result from zircon SHRIMP U-Pb dating and its tectonic implications[J]. Acta Petrologica Sinica, 2004,20(3):621-626.
[26]	Zhang S H, Zhao Y, Song B, et al. Contrasting Late Carboniferous and Late Permian-Middle Triassic intrusive suites from the northern margin of the North China craton:Geochronology, petrogenesis, and tectonic implications[J]. GSABulletin, 2009,121(1/2):181-200.
[27]	Zhang S H, Zhao Y, Liu X C, 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(1/4):229-246.
[28]	Ducea M. The California arc:Thick granitic batholiths, eclogitic residues, lithospheric-scale thrusting, and magmatic flare-ups[J]. GSA Today, 2001,11(11):4-10.
[29]	Lackey J S, Valley J W, Saleeby J B. Supracrustal input to magmas in the deep crust of Sierra Nevada batholith:Evidence from high- δ18O zircon[J]. Earth and Planetary Science Letters, 2005,235(1/2): 315-330.
[30]	倪志耀,翟明国,王仁民,等. 华北古陆块北缘中段发现晚古生代退变榴辉岩[J]. 科学通报, 2004,49(6):585-591. Ni Z Y, Zhai M G, Wang R M, et al. Discovery of Late Paleozoic retrograded eclogites from the middle part of the northern margin of North China Craton[J]. Chinese Science Bulletin, 2004,49(6):600- 606.
[31]	罗镇宽,苗来成,关康,等. 冀东都山花岗岩基及相关花岗斑岩脉SHRIMP锆石U-Pb法定年及其意义[J]. 地球化学, 2003,32(2): 173-180. Luo Z K, Miao L C, Guan K, et al. SHRIMP U-Pb zircon dating of the Dushan granitic batholiths and related granite-porphyry dyke, eastern Hebei Province, China, and their geological significance[J]. Geochimica, 2003,32(2):173-180.
[32]	罗镇宽,李俊建,关康,等. 辽宁凌源柏杖子金矿区花岗岩SHRIMP锆石U-Pb年龄[J]. 地质调查与研究, 2004,27(2):82-85, 128. Luo Z K, Li J J, Guan K, et al. SHRIMP zircon U-Pb age of the granite at Baizhangzi gold field in Lingyuan, Liaoning Province[J]. Geological Survey and Research, 2004,27(2):82-85, 128.
[33]	马芳,穆治国,刘玉琳. 河北滦平球状闪长岩年代学及其地质意义[J]. 地质论评, 2004,50(4):360-364. Ma F, Mu Z G, Liu Y L. Geochronology and geologic significance of the orbicular dioritic rocks in Luanping, Hebei Province[J]. Geological Review, 2004,50(4):360-364.
[34]	张拴宏,赵越,刘健,等. 华北地块北缘晚古生代-中生代花岗岩体侵位深度及其构造意义[J]. 岩石学报, 2007,23(3):625-638. Zhang S H, Zhao Y, Liu J, et al. Emplacement depths of the Late Paleozoic-Mesozoic granitoid intrusions from the northern North China block and their tectonic implications[J]. Acta Petrologica Sinica, 2007,23(3):625-638.
[35]	田伟,陈斌,刘超群,等. 冀北小张家口超基性岩体的锆石U-Pb年龄和Hf同位素组成[J]. 岩石学报, 2007,23(3):583-590. Tian W, Chen B, Liu C Q, et al. Zircon U-Pb age and Hf isotopic composition of the Xiaozhangjiakou ultramafic pluton in northern Hebei[J]. Acta Petrologica Sinica, 2007,23(3):583-590.
[36]	Zhang S H, Zhao Y, Song B, 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(2):451-463.