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Pulsed Mesozoic exhumation in Northeast Asia: New constraints from zircon U-Pb and apatite U-Pb, fission track and (U-Th)/He analyses in the Zhangguangcai Range, NE China

文献类型：期刊论文

作者Wang, Nan4,5; Zhang, Zhiyong4; Malusa, Marco G.1; Wu, Lin4; Chew, David2; Zhang, Jien4; Xiang, Dunfeng4,5; Xiao, Wenjiao3
刊名TECTONOPHYSICS
出版日期2021-11-05
卷号818页码:17
关键词Northeast China Central Zhangguangcai Range U-Pb geochronology Low-temperature thermochronology Mudanjiang Ocean Pulsed Mesozoic exhumation
ISSN号0040-1951
DOI10.1016/j.tecto.2021.229075
英文摘要Northeast Asia located at the margin of the Paleo-Pacific/Pacific plate provides a detailed record of subduction-related omgenic activity. In order to shed light on Mesozoic-Cenozoic tectonic processes arising from the complex interaction and juxtaposition of multiple tectonic domains, we performed zircon U-Pb and apatite U-Pb, fission-track (FT) and (U-Th)/He analyses in the Zhangguangcai Range, a major mountain range in northeastern Asia. Our zircon and apatite U-Pb results indicate that most granites in the Zhangguangcai Range were emplaced at shallow crustal levels in the early Jurassic (similar to 200-173 Ma) along with a minor amount of Triassic granites (similar to 232 Ma). Volcanic rocks of the Maoershan and Ningyuancun formations were erupted at similar to 190-175 Ma and similar to 182-177 Ma, respectively. This Early Mesozoic magmatic activity is related to subduction of the Mudanjiang oceanic plate that separated the Jiamusi and Songliao blocks. Apatite FT analysis of granites and volcanic rocks reveals three groups of cooling ages clustering at similar to 193-171 Ma, similar to 158-129 Ma and similar to 118-102 Ma, while AHe analysis of granites yielded three groups of cooling ages at similar to 149-135 Ma, similar to 106-85 Ma and similar to 57-48 Ma. Based on these data and thermal history modelling, we propose that the central Zhangguangcai Range experienced episodic, multi-stage exhumation at shallow crustal levels since the Jurassic. Early-Middle Jurassic exhumation took place during the closure of the Mudanjiang Ocean, which resulted in unroofing of granites in the central Zhangguangcai Range and topographic growth of the Songliao block. Late Jurassic-Early Cretaceous exhumation occurred within an extensional tectonic setting, which has previously been documented across northeast Asia. Such exhumation could have been linked to lithosphere delamination and resulted in basin and range topography style, prior to the change in subduction parameters of the Paleo-Pacific plate and/or collision and strike-slip translation of the Okhotomorsk block in the Late Cretaceous.
WOS关键词CONTINENTAL-MARGIN EVOLUTION ; SONGLIAO BASIN ; HEILONGJIANG COMPLEX ; TECTONIC EVOLUTION ; GEOCHEMICAL CONSTRAINTS ; ACCRETIONARY COMPLEX ; LU-HF ; CENOZOIC EXHUMATION ; ADJACENT REGIONS ; RADIATION-DAMAGE
资助项目"Strategic Priority Research Program (B)" of the Chinese Academy of Sciences[XDB18030103] ; National Natural Science Foundation of China[92055213] ; National Natural Science Foundation of China[91855207] ; National Natural Science Foundation of China[41888101] ; Science Foundation Ireland[13/RC/2092] ; Science Foundation Ireland[13/RC/2092_P2]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000703690400007
出版者ELSEVIER
资助机构"Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Science Foundation Ireland ; Science Foundation Ireland ; Science Foundation Ireland ; Science Foundation Ireland ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Science Foundation Ireland ; Science Foundation Ireland ; Science Foundation Ireland ; Science Foundation Ireland ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Science Foundation Ireland ; Science Foundation Ireland ; Science Foundation Ireland ; Science Foundation Ireland ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; "Strategic Priority Research Program (B)" of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Science Foundation Ireland ; Science Foundation Ireland ; Science Foundation Ireland ; Science Foundation Ireland
源URL[http://ir.iggcas.ac.cn/handle/132A11/102703]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Zhang, Zhiyong
作者单位1.Univ Milano Bicocca, Dept Earth & Environm Sci, Lab Provenance Studies, Piazza Sci 4, I-20126 Milan, Italy
2.Trinity Coll Dublin, Sch Nat Sci, Dept Geol, Dublin 2, Ireland
3.Chinese Acad Sci, Xinjiang Res Ctr Mineral Resources, Xinjiang Inst Ecol & Geog, Urumqi 830011, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714		 Wang, Nan,Zhang, Zhiyong,Malusa, Marco G.,et al. Pulsed Mesozoic exhumation in Northeast Asia: New constraints from zircon U-Pb and apatite U-Pb, fission track and (U-Th)/He analyses in the Zhangguangcai Range, NE China[J]. TECTONOPHYSICS,2021,818:17.
APA Wang, Nan.,Zhang, Zhiyong.,Malusa, Marco G..,Wu, Lin.,Chew, David.,...&Xiao, Wenjiao.(2021).Pulsed Mesozoic exhumation in Northeast Asia: New constraints from zircon U-Pb and apatite U-Pb, fission track and (U-Th)/He analyses in the Zhangguangcai Range, NE China.TECTONOPHYSICS,818,17.
MLA Wang, Nan,et al."Pulsed Mesozoic exhumation in Northeast Asia: New constraints from zircon U-Pb and apatite U-Pb, fission track and (U-Th)/He analyses in the Zhangguangcai Range, NE China".TECTONOPHYSICS 818(2021):17.

入库方式： OAI收割

来源：地质与地球物理研究所

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