中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Geological relation of Late Archean lithologic units in Northwest Hebei, North China Craton: Implication for building of early continental crust

文献类型:期刊论文

作者Peng Peng; Li Yun; Liu Fu; Wang Fang
刊名ACTA PETROLOGICA SINICA
出版日期2012-11-01
卷号28期号:11页码:3531-3544
关键词North China Craton Late Archean Crust structure Volcano-sedimentary sequences grey gneisses (TTG gneisses) Hongqiyingzi Group
ISSN号1000-0569
文献子类Article
英文摘要In Northwest Hebei Province, North China Craton, the Late Archean units include grey gneisses-dominated Sanggan and Chongli complexes and amphibolite-facies volcano-sedimentary sequence, the Hongqiyingzi Group. In this paper, zircon grains from a meta-basaltic-andesite sample (amphibole plagioclase gneiss) from the Hongqiyingzi Group in Huangtuyao-Wushijia area, Shangyi, was dated using LA-MC-ICPMS method. A weighted mean Pb-207/Pb-206 age of 2528 +/- 12Ma (2 sigma, MSWD = 0.1, n = 34) was obtained, and this age is interpreted as igneous age of the rock. Although this age is close to the ages of the grey gneisses in this area, field relations clearly show that the Hongqiyingzi Group has formed earlier. In the grey gneiss domain, pieces of the Hongqiyingzi Group and other meta-gabbros appear as sheets, lens or "dyke"-like bands. These lens and bands sometimes have numbers of lined smaller lens around the main bodies, with no fine-grained margins and intrusive branches, which can distinguish from the Paleoproterozoic mafic dykes (also metamorphosed) in this same area. These gabbroic sheets could be roots or partly the magma chamber relics of the Hongqiyingzi Group, or they could also be partly the remanents of ancient crust. Element and isotope geochemistry show that the volcanics are akin of grey gneisses or dioritic intrusions in the grey gneisses in this area. Both geological relations and geochemistry show that these volcanic rocks may have similar origins with the grey gneisses and dioritic rocks. According to the geological relationships of the Late Archean units in this area, the volcano-sedimentary sequence (the Hongqiyingzi Group) and the grey gneiss complex (Sanggan and Chongli complexes) composed a 2-dimension Late Archean crust structure. Identifying the spatial continuity of such crustal structure, as well as the time and material evolution of the related units, can reveal the forming mechanism of Late Archean continental crust in the North China Craton.
WOS关键词HIGH-PRESSURE GRANULITES ; PB ZIRCON GEOCHRONOLOGY ; GREENSTONE-BELT ; LU-HF ; EVOLUTION ; TECTONICS ; COMPLEX ; MANTLE ; GEOCHEMISTRY ; PETROGENESIS
WOS研究方向Geology
语种英语
WOS记录号WOS:000312572600008
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/84568]  
专题中国科学院地质与地球物理研究所
通讯作者Peng Peng
作者单位Chinese Acad Sci, Inst Geol & Geophys, Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Peng Peng,Li Yun,Liu Fu,et al. Geological relation of Late Archean lithologic units in Northwest Hebei, North China Craton: Implication for building of early continental crust[J]. ACTA PETROLOGICA SINICA,2012,28(11):3531-3544.
APA Peng Peng,Li Yun,Liu Fu,&Wang Fang.(2012).Geological relation of Late Archean lithologic units in Northwest Hebei, North China Craton: Implication for building of early continental crust.ACTA PETROLOGICA SINICA,28(11),3531-3544.
MLA Peng Peng,et al."Geological relation of Late Archean lithologic units in Northwest Hebei, North China Craton: Implication for building of early continental crust".ACTA PETROLOGICA SINICA 28.11(2012):3531-3544.

入库方式: OAI收割

来源:地质与地球物理研究所

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