LATE NEOARCHEAN SUPRACRUSTAL ROCKS FROM THE ANSHAN-BENXI TERRANE, NORTH CHINA CRATON: NEW GEODYNAMIC IMPLICATIONS FROM THE GEOCHEMICAL RECORD
Wang, Changle1; Peng, Zidong1,2; Tong, Xiaoxue1,2; Huang, Hua1; Zheng, Mengtian1,2; Zhang, Lianchang1,2; Zhai, Mingguo1
刊名AMERICAN JOURNAL OF SCIENCE
2017-12-01
卷号317期号:10页码:1095-1148
关键词Neoarchean North China Craton Anshan-benxi Supracrustal Rocks Geochemistry Geodynamic Setting
ISSN号0002-9599
DOI10.2475/10.2017.02
文献子类Article
英文摘要The late Neoarchean supracrustal rocks of the Anshan-Benxi (AnBen) terrane in the northeastern part of the North China Craton (NCC) have important regional tectonostratigraphic implications for the development of large-scale banded iron formations (BIFs). These supracrustal rocks underwent polyphase deformation and upper greenschist to upper amphibolite facies metamorphism and are subdivided into two main lithotectonic units in terms of differing ages, metamorphic grades, and lithological assemblages: the Benxi unit (similar to 2.56 - 2.53 Ga) composed of tholeiitic to transitional mafic rocks with minor siliciclastic sedimentary rocks, and the Anshan unit (similar to 2.53-2.51 Ga) consisting of siliciclastic sedimentary rocks with minor tholeiitic mafic rocks. In this study, we report the results of field investigations and petrographic, whole-rock major and trace element geochemical and Sm-Nd isotopic analyses, as well as zircon U-Pb-Hf-O isotopic analyses for these volcano-sedimentary rocks, and integrate the results with previously published data to provide a new geodynamic synthesis for the setting of the BIFs.
WOS关键词ZIRCON U-PB ; BANDED IRON-FORMATIONS ; NORTHWESTERN SUPERIOR PROVINCE ; BARBERTON GREENSTONE-BELT ; ARCHEAN CRUSTAL EVOLUTION ; BACK-ARC BASIN ; LIAONING PROVINCE ; TRACE-ELEMENT ; CONTINENTAL-CRUST ; VOLCANIC-ROCKS
WOS研究方向Geology
语种英语
出版者AMER JOURNAL SCIENCE
WOS记录号WOS:000422717500002
资助机构CPSF-CAS Joint Foundation for Excellent Postdoctoral Fellows(2015LH0004) ; CPSF-CAS Joint Foundation for Excellent Postdoctoral Fellows(2015LH0004) ; National Natural Science Foundation of China(41572076 ; National Natural Science Foundation of China(41572076 ; 41602085) ; 41602085) ; CPSF-CAS Joint Foundation for Excellent Postdoctoral Fellows(2015LH0004) ; CPSF-CAS Joint Foundation for Excellent Postdoctoral Fellows(2015LH0004) ; National Natural Science Foundation of China(41572076 ; National Natural Science Foundation of China(41572076 ; 41602085) ; 41602085) ; CPSF-CAS Joint Foundation for Excellent Postdoctoral Fellows(2015LH0004) ; CPSF-CAS Joint Foundation for Excellent Postdoctoral Fellows(2015LH0004) ; National Natural Science Foundation of China(41572076 ; National Natural Science Foundation of China(41572076 ; 41602085) ; 41602085) ; CPSF-CAS Joint Foundation for Excellent Postdoctoral Fellows(2015LH0004) ; CPSF-CAS Joint Foundation for Excellent Postdoctoral Fellows(2015LH0004) ; National Natural Science Foundation of China(41572076 ; National Natural Science Foundation of China(41572076 ; 41602085) ; 41602085)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/82492]  
专题中国科学院地质与地球物理研究所
通讯作者Wang, Changle; Zhang, Lianchang
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Wang, Changle,Peng, Zidong,Tong, Xiaoxue,et al. LATE NEOARCHEAN SUPRACRUSTAL ROCKS FROM THE ANSHAN-BENXI TERRANE, NORTH CHINA CRATON: NEW GEODYNAMIC IMPLICATIONS FROM THE GEOCHEMICAL RECORD[J]. AMERICAN JOURNAL OF SCIENCE,2017,317(10):1095-1148.
APA Wang, Changle.,Peng, Zidong.,Tong, Xiaoxue.,Huang, Hua.,Zheng, Mengtian.,...&Zhai, Mingguo.(2017).LATE NEOARCHEAN SUPRACRUSTAL ROCKS FROM THE ANSHAN-BENXI TERRANE, NORTH CHINA CRATON: NEW GEODYNAMIC IMPLICATIONS FROM THE GEOCHEMICAL RECORD.AMERICAN JOURNAL OF SCIENCE,317(10),1095-1148.
MLA Wang, Changle,et al."LATE NEOARCHEAN SUPRACRUSTAL ROCKS FROM THE ANSHAN-BENXI TERRANE, NORTH CHINA CRATON: NEW GEODYNAMIC IMPLICATIONS FROM THE GEOCHEMICAL RECORD".AMERICAN JOURNAL OF SCIENCE 317.10(2017):1095-1148.
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