Tectonic history of the Huangsong tectonic terrains in the Khanka Massif in the easternmost Central Asian Orogenic Belt: Constraints from detrital zircon U-Pb geochronology

被引:3
作者
Zhang, Siwen [1 ]
Wang, Feng [1 ,2 ]
Xu, Wenliang [1 ,2 ]
Gao, Fuhong [1 ]
Tang, Jie [1 ,2 ]
机构
[1] Jilin Univ, Coll Earth Sci, 2199 Jianshe St, Changchun 130061, Peoples R China
[2] Minist Land & Resources China, Key Lab Mineral Resources Evolut Northeast Asia, Changchun, Peoples R China
基金
中国国家自然科学基金;
关键词
Central Asian Orogenic Belt; Khanka Massif; Huangsong Group; Detrital zircon; Tectonic history; SONGNEN-ZHANGGUANGCAI RANGE; NE CHINA IMPLICATIONS; LA-ICP-MS; CARBONIFEROUS IGNEOUS ROCKS; LU-HF ISOTOPES; JIAMUSI MASSIF; VOLCANIC-ROCKS; NORTH CHINA; HEILONGJIANG PROVINCE; GRANITIC MAGMATISM;
D O I
10.1016/j.gr.2021.07.002
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Khanka Massif, as the easternmost micro-massif of the Central Asian Orogenic Belt, its tectonic attributes and Paleozoic tectonic evolution remain controversial. In this paper, we present detrital zircon U-Pb age data for sedimentary rocks from the Huangsong Group, in order to provide constraints in this regard. The Huangsong Group has previously been described as the Precambrian basement of the Khanka Massif, consists of slightly metamorphosed sedimentary rocks, and from bottom to top is divided into the Yangmu and Yanwangdian suites. Unexpectedly, the depositional ages of the Yangmu suite are (from bottom to top) 220-205 Ma, 249-239 Ma, and 509-485 Ma. The depositional ages of the Yanwangdian suite are (from bottom to top) 426-390 Ma and 232-220 Ma. Clearly, the rocks do not have a logical stratigraphic sequence and, therefore, we propose that the "Huangsong Group" represents a stack of tectonic terrains with diverse ages (early Paleozoic to early Mesozoic) rather than a continuous sedimentary sequence. The potential sediment sources were mainly a nearby magmatic arc and batholiths, because the zircons are euhedral-subhedral, exhibit well-developed oscillatory zoning, and have high Th/U ratios. The occurrence of Precambrian detrital zircon grains implies the existence of remnants of Precambrian basement along the western margin of the Khanka Massif in the early Paleozoic. A comparison of magmatism in the regional massifs revealed there was a tectonic affinity between the western margin of the Khanka Massif and eastern margin of the Songnen-Zhangguangcai Range Massif in the Paleozoic. Based on the detrital zircon age populations and trace element contents, we conclude that the western Khanka Massif experienced a change from a stable to an active margin setting during the late Paleozoic, which was caused by subduction of the Paleo-Asian oceanic lithosphere. (c) 2021 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:149 / 162
页数:14
相关论文
共 50 条
[41]   Crustal evolution in the South Tianshan Terrane: Constraints from detrital zircon geochronology and implications for continental growth in the Central Asian Orogenic Belt [J].
Huang, He ;
Zhang, Zhaochong ;
Santosh, M. ;
Cheng, Zhiguo ;
Wang, Tao .
GEOLOGICAL JOURNAL, 2019, 54 (03) :1379-1400
[42]   Tectonic attributes and Late Paleozoic geological background of Mian-Lue belt in the southern margin of Qinling: Constraints from U-Pb geochronology of zircon [J].
Li XiaoBing ;
Pei XianZhi ;
Li ZuoChen ;
Li RuiBao ;
Pei Lei ;
Gao Feng ;
Wang Meng .
ACTA PETROLOGICA SINICA, 2021, 37 (05) :1444-1468
[43]   Provenance and tectonic settings of the Early Silurian clastic rocks in the southeast Upper Yangtze region: Constraints from the whole-rock geochemistry and detrital zircon U-Pb geochronology [J].
Ren, Peng ;
Mou, Chuanlong ;
Zhou, Gang ;
Wang, Qiyu ;
Wang, Xiuping .
JOURNAL OF ASIAN EARTH SCIENCES, 2023, 250
[44]   Petrography, geochemistry, and U-Pb detrital zircon dating of early Permian sedimentary rocks from the North Flank of the North China Craton: Implications for the late Palaeozoic tectonic evolution of the eastern Central Asian Orogenic Belt [J].
Luo, Zhiwen ;
Zhang, Zhicheng ;
Li, Ke ;
Li, Jianfeng ;
Tang, Wenhao ;
Xu, Bei .
INTERNATIONAL GEOLOGY REVIEW, 2016, 58 (07) :787-806
[45]   Petrology, Geochemistry and Zircon U-Pb Geochronology of the Xiangshan Group in the Eastern Hexi Corridor Belt: Implications for Provenance and Tectonic Evolution [J].
Zhao, Xiaochen ;
Liu, Chiyang ;
Wang, Jianqiang ;
Duan, Liang ;
Zhao, Yan ;
Zhang, Qihang ;
Luo, Wei .
ACTA GEOLOGICA SINICA-ENGLISH EDITION, 2017, 91 (05) :1680-1703
[46]   Petrogenesis and tectonic implications of the Early Paleozoic intermediate and mafic intrusions in the South Qinling Belt, Central China: Constraints from geochemistry, zircon U-Pb geochronology and Hf isotopes [J].
Wang, Ruirui ;
Xu, Zhiqin ;
Santosh, M. ;
Liang, Fenghua ;
Fu, Xuehai .
TECTONOPHYSICS, 2017, 712 :270-288
[47]   U-Pb geochronology of detrital and inherited zircons in the Yidun arc belt, eastern Tibet Plateau and its tectonic implications [J].
Tao Wu ;
Long Xiao ;
Changqian Ma .
Journal of Earth Science, 2016, 27 :461-473
[48]   Metamorphic patterns and zircon U-Pb dating of the Xilingol complex in Inner Mongolia, China: Implications for rifting metamorphism and tectonic evolution in eastern Central Asian Orogenic Belt [J].
Cao, Da-Di ;
Wang, Yi-Cun ;
Yin, Lu ;
Xu, Bei .
LITHOS, 2022, 428
[49]   U-Pb Geochronology of Detrital and Inherited Zircons in the Yidun Arc Belt, Eastern Tibet Plateau and Its Tectonic Implications [J].
Wu, Tao ;
Xiao, Long ;
Ma, Changqian .
JOURNAL OF EARTH SCIENCE, 2016, 27 (03) :461-473
[50]   U-Pb Geochronology of Detrital and Inherited Zircons in the Yidun Arc Belt, Eastern Tibet Plateau and Its Tectonic Implications [J].
Tao Wu ;
Long Xiao ;
Changqian Ma .
Journal of Earth Science, 2016, 27 (03) :461-473