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U-Pb Dating and Lu-Hf Isotopes of Detrital Zircons From the Southern Sikhote-Alin Orogenic Belt, Russian Far East: Tectonic Implications for the Early Cretaceous Evolution of the Northwest Pacific Margin

文献类型：期刊论文

作者Liu, Kai1,2; Zhang, Jinjiang1; Wilde, Simon A.2; Liu, Shiran1; Guo, Feng3; Kasatkin, Sergey A.4; Golozoubov, Vladimir V.4; Ge, Maohui1; Wang, Meng5; Wang, Jiamin6
刊名TECTONICS
出版日期2017-11-01
卷号36期号:11页码:2555-2598
关键词Sikhote-alin Strike-slip Detrital Zircon Early Cretaceous Paleo-pacific
ISSN号0278-7407
DOI10.1002/2017TC004599
文献子类Article
英文摘要The Sikhote-Alin orogenic belt in Russian Far East is comprised of several N-S trending belts, including the Late Jurassic to Early Cretaceous accretionary prisms and turbidite basin which are now separated by thrusts and strike-slip faults. The origin and collage of the belts have been studied for decades. However, the provenance of the belts remains unclear. Six sandstone samples were collected along a 200km long east-west traverse across the major belts in the southern Sikhote-Alin for U-Pb dating and Lu-Hf isotope analysis to constrain the provenance and evaluate the evolution of the northwest Pacific margin at this time. The result reveals that the sediments from the main Samarka belt was mainly from the adjacent Bureya-Jiamusi-Khanka Block (BJKB); the eastern Samarka belt and the Zhuravlevka turbidite basin were supplied by detritus from both the North China Craton (NCC) and the BJKB; the Taukha belt was mainly fed by sediments from the NCC; whereas the data from the Sergeevka nappes are insufficient to resolve their provenance. In the Late Jurassic to Early Cretaceous, collision and subduction was important in the initial collage of most belts in Sikhote-Alin. However, merely E-W trending collage cannot explain the increasing importance of the NCC provenance from west to east. It is proposed that the main Samarka belt was located adjacent to the BJKB when deposited, whereas the other belts were farther south to accept the materials from the NCC. Sinistral strike-slip faulting transported the eastern belts northward after their initial collage by thrusting.
WOS关键词ARCHEAN CRUSTAL EVOLUTION ; NE CHINA CONSTRAINTS ; JURASSIC ACCRETIONARY PRISM ; PALEO-ASIAN OCEAN ; I-TYPE GRANITES ; JIAMUSI MASSIF ; NORTHEASTERN CHINA ; KOREAN PENINSULA ; SW JAPAN ; METAMORPHIC COMPLEX
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000418334800013
出版者AMER GEOPHYSICAL UNION
资助机构State Key Program of National Natural Science Foundation of China(41730210) ; State Key Program of National Natural Science Foundation of China(41730210) ; Major State Basic Research Development Program of China(2013 CB429804) ; Major State Basic Research Development Program of China(2013 CB429804) ; Fundamental Research Funds for the Central Universities(310827161010) ; Fundamental Research Funds for the Central Universities(310827161010) ; State Key Program of National Natural Science Foundation of China(41730210) ; State Key Program of National Natural Science Foundation of China(41730210) ; Major State Basic Research Development Program of China(2013 CB429804) ; Major State Basic Research Development Program of China(2013 CB429804) ; Fundamental Research Funds for the Central Universities(310827161010) ; Fundamental Research Funds for the Central Universities(310827161010) ; State Key Program of National Natural Science Foundation of China(41730210) ; State Key Program of National Natural Science Foundation of China(41730210) ; Major State Basic Research Development Program of China(2013 CB429804) ; Major State Basic Research Development Program of China(2013 CB429804) ; Fundamental Research Funds for the Central Universities(310827161010) ; Fundamental Research Funds for the Central Universities(310827161010) ; State Key Program of National Natural Science Foundation of China(41730210) ; State Key Program of National Natural Science Foundation of China(41730210) ; Major State Basic Research Development Program of China(2013 CB429804) ; Major State Basic Research Development Program of China(2013 CB429804) ; Fundamental Research Funds for the Central Universities(310827161010) ; Fundamental Research Funds for the Central Universities(310827161010)
源URL[http://ir.iggcas.ac.cn/handle/132A11/82378]  
专题中国科学院地质与地球物理研究所
通讯作者Zhang, Jinjiang
作者单位1.Peking Univ, Key Lab Orogen & Crustal Evolut, Minist Educ, Beijing, Peoples R China
2.Curtin Univ, Inst Geosci Res, Dept Appl Geol, Perth, WA, Australia
3.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Marginal Sea Geol, Guangzhou, Guangdong, Peoples R China
4.Russian Acad Sci, Far East Geol Inst, Far East Branch, Vladivostok, Russia
5.Changan Univ, Sch Earth Sci & Resources, Key Lab Study Focused Magmatism & Giant Ore Depos, Xian, Shaanxi, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
推荐引用方式
GB/T 7714		 Liu, Kai,Zhang, Jinjiang,Wilde, Simon A.,et al. U-Pb Dating and Lu-Hf Isotopes of Detrital Zircons From the Southern Sikhote-Alin Orogenic Belt, Russian Far East: Tectonic Implications for the Early Cretaceous Evolution of the Northwest Pacific Margin[J]. TECTONICS,2017,36(11):2555-2598.
APA Liu, Kai.,Zhang, Jinjiang.,Wilde, Simon A..,Liu, Shiran.,Guo, Feng.,...&Wang, Jiamin.(2017).U-Pb Dating and Lu-Hf Isotopes of Detrital Zircons From the Southern Sikhote-Alin Orogenic Belt, Russian Far East: Tectonic Implications for the Early Cretaceous Evolution of the Northwest Pacific Margin.TECTONICS,36(11),2555-2598.
MLA Liu, Kai,et al."U-Pb Dating and Lu-Hf Isotopes of Detrital Zircons From the Southern Sikhote-Alin Orogenic Belt, Russian Far East: Tectonic Implications for the Early Cretaceous Evolution of the Northwest Pacific Margin".TECTONICS 36.11(2017):2555-2598.

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来源：地质与地球物理研究所

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