Early-Middle Paleozoic subduction-collision history of the south-eastern Central Asian Orogenic Belt: Evidence from igneous and metasedimentary rocks of central Jilin Province, NE China

doi:10.1016/j.lithos.2015.12.010

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 岩石圈演化国家重点实验室

	Early-Middle Paleozoic subduction-collision history of the south-eastern Central Asian Orogenic Belt: Evidence from igneous and metasedimentary rocks of central Jilin Province, NE China
	Pei, Fu-Ping 1; Zhang, Ying 1; Wang, Zhi-Wei 1; Cao, Hua-Hua 2; Xu, Wen-Liang 1,3; Wang, Zi-Jin 1; Wang, Feng 1; Yang, Chuan 4
刊名	LITHOS
	2016-09-15
卷号	261 页码:164-180
关键词	Early-middle Paleozoic Central Asian Orogenic Belt Igneous Rock Supra-subduction Zone
DOI	10.1016/j.lithos.2015.12.010
文献子类	Article
英文摘要	To constrain the Early-Middle Paleozoic tectonic evolution of the south-eastern segment of the Central Asian Orogenic Belt (CAOB), we undertook zircon U-Pb dating and analyzed major and trace elements and zircon Hf isotope compositions of Late Cambrian to Middle Devonian igneous and metasedimentary rocks in central Jilin Province, NE China. LA-ICP-MS zircon U-Pb dating indicates that the Early-Middle Paleozoic magmatism in central Jilin Province can be divided into four episodes: Late Cambrian (ca. 493 Ma), Middle Ordovician (ca. 467 Ma), Late Ordovician-Early Silurian (ca. 443 Ma), and Late Silurian-Middle Devonian (425-396 Ma). The progression from subduction initiation to maturity is recorded by Late Cambrian low-K tholeiitic meta-diabase, Middle Ordovician medium-K calc-alkaline pyroxene andesite, and Late Ordovician to Early Silurian low-K tonalite, which all have subduction-related characteristics and formed in an evolving supra-subduction zone setting. Late Silurian to Middle Devonian calc-alkaline igneous rocks, with the lithological association of granodiorite, monzogranite, rhyolite, dacite, and trachydacite, show progressively increasing K2O contents from medium K to shoshonite series. Furthermore, the Early-Middle Devonian monzogranites are characterized by high K2O, Sr/Y, and [La/Yb](N) values, indicating they were generated by the melting of thickened lower crust. These results suggest a transition from subduction to post-orogenic setting during the Late Silurian-Middle Devonian. Our interpretation is supported by the maximum age of molasse deposition in the Zhangjiatun member of the Xibiehe Formation. Overall, we suggest that Late Cambrian tholeiitic meta-diabase, Middle Ordovician pyroxene andesite, and Late Ordovician-Early Silurian tonalite formed above the northward-subducting and simultaneously seaward-retreating of Paleo-Asian Ocean plate. Subsequently, the northern arc collided with the North China Craton and post-orogenic extension occurred during the Late Silurian-Middle Devonian. (C) 2016 Elsevier B.V. All rights reserved.
WOS关键词	U-PB GEOCHRONOLOGY ; LA-ICP-MS ; NORTH CHINA ; INNER-MONGOLIA ; VOLCANIC-ROCKS ; TECTONIC EVOLUTION ; DETRITAL ZIRCONS ; GEOCHEMISTRY ; PETROGENESIS ; ISOTOPE
WOS研究方向	Geochemistry & Geophysics ; Mineralogy
语种	英语
WOS记录号	WOS:000381833500010
资助机构	National Basic Research Program of China(2013CB429802) ; National Basic Research Program of China(2013CB429802) ; National Natural Science Foundation of China(41172057 ; National Natural Science Foundation of China(41172057 ; China Geological Survey(1212011085480 ; China Geological Survey(1212011085480 ; Opening Foundation of the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences(GPMR201303) ; Opening Foundation of the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences(GPMR201303) ; 41572043 ; 41572043 ; 12120113098200) ; 12120113098200) ; 41330206 ; 41330206 ; 41272075) ; 41272075) ; National Basic Research Program of China(2013CB429802) ; National Basic Research Program of China(2013CB429802) ; National Natural Science Foundation of China(41172057 ; National Natural Science Foundation of China(41172057 ; China Geological Survey(1212011085480 ; China Geological Survey(1212011085480 ; Opening Foundation of the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences(GPMR201303) ; Opening Foundation of the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences(GPMR201303) ; 41572043 ; 41572043 ; 12120113098200) ; 12120113098200) ; 41330206 ; 41330206 ; 41272075) ; 41272075)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/53371]
专题	地质与地球物理研究所_岩石圈演化国家重点实验室
作者单位	1.Jilin Univ, Coll Earth Sci, 2199 Jianshe St, Changchun 130061, Jilin, Peoples R China 2.Ocean Univ China, Coll Marine Geosci, Qingdao 266003, Peoples R China 3.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, POB 9825, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Pei, Fu-Ping,Zhang, Ying,Wang, Zhi-Wei,et al. Early-Middle Paleozoic subduction-collision history of the south-eastern Central Asian Orogenic Belt: Evidence from igneous and metasedimentary rocks of central Jilin Province, NE China[J]. LITHOS,2016,261:164-180.
APA	Pei, Fu-Ping.,Zhang, Ying.,Wang, Zhi-Wei.,Cao, Hua-Hua.,Xu, Wen-Liang.,...&Yang, Chuan.(2016).Early-Middle Paleozoic subduction-collision history of the south-eastern Central Asian Orogenic Belt: Evidence from igneous and metasedimentary rocks of central Jilin Province, NE China.LITHOS,261,164-180.
MLA	Pei, Fu-Ping,et al."Early-Middle Paleozoic subduction-collision history of the south-eastern Central Asian Orogenic Belt: Evidence from igneous and metasedimentary rocks of central Jilin Province, NE China".LITHOS 261(2016):164-180.