中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Coexisting Late Cenozoic Potassic and Sodic Basalts in NE China: Role of Recycled Oceanic Components in Intraplate Magmatism and Mantle Heterogeneity

文献类型:期刊论文

作者Lei, Ming1,2,4; Guo, Zhengfu1,2,4; Zhao, Wenbin1,2,4; Zhang, Maoliang1,2,3,4; Ma, Lin1,2,4
刊名LITHOSPHERE
出版日期2020-06-01
卷号2020期号:1页码:28
ISSN号1941-8264
DOI10.2113/2020/8875012
英文摘要This study presents an integrated geochemical study of the Wudalianchi-Erkeshan potassic basalts and Halaha sodic basalts of NE China, and uses these data to further our understanding of the petrogenetic relationships between the coeval potassic and sodic basalts in this region. The potassic basalts with high concentrations of K2O have arc-like trace-element compositions and enriched Sr-Nd-Hf isotopic compositions with unradiogenic Pb-206/Pb-204 values (16.77-16.90). In contrast, the sodic basalts with high concentrations of Na2O have OIB-like trace-element compositions and depleted Sr-Nd-Hf isotopic compositions with radiogenic Pb-206/Pb-204 values (18.27-18.40). These data suggest that the potassic and sodic basalts were derived from mixed depleted mid-ocean-ridge basalt mantle (DMM) and enriched mantle source end-members, where the enriched end-members are ancient sediment for the potassic basalts and Pacific oceanic crust for the sodic basalts. The combined geophysical and geochemical data indicate that these two enriched end-members are located in the mantle transition zone. We propose that partial melting of upwelling asthenospheric mantle comprising ambient DMM and recycled materials shifting from the ancient sediment to the Pacific oceanic crust could have produced the coeval potassic and sodic basalts in NE China. The proposed mantle sources for the potassic and sodic basalts indicate that the upper mantle beneath NE China was highly heterogeneous during late Cenozoic.
WOS关键词ULTRAPOTASSIC VOLCANIC-ROCKS ; SPINEL PERIDOTITE XENOLITHS ; PARTIAL MELTING EXPERIMENTS ; XINGAN RANGE EVIDENCE ; ASIAN OROGENIC BELT ; SINO-KOREAN CRATON ; CHAOER RIVER AREA ; LITHOSPHERIC MANTLE ; TRACE-ELEMENT ; TRANSITION-ZONE
资助项目Strategic Priority Research Program of the Chinese Academy of Sciences[XDB26000000] ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences[QYZDY-SSW-DQC030] ; Natural Science Foundation of China[41702361] ; Natural Science Foundation of China[41572321]
WOS研究方向Geochemistry & Geophysics ; Geology
语种英语
WOS记录号WOS:000617908500034
出版者GEOSCIENCEWORLD
资助机构Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Strategic Priority Research Program of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of the Chinese Academy of Sciences ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China ; Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/100051]  
专题地质与地球物理研究所_中国科学院新生代地质与环境重点实验室
通讯作者Guo, Zhengfu
作者单位1.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Tianjin Univ, Inst Surface Earth Syst Sci, Tianjin 300072, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Lei, Ming,Guo, Zhengfu,Zhao, Wenbin,et al. Coexisting Late Cenozoic Potassic and Sodic Basalts in NE China: Role of Recycled Oceanic Components in Intraplate Magmatism and Mantle Heterogeneity[J]. LITHOSPHERE,2020,2020(1):28.
APA Lei, Ming,Guo, Zhengfu,Zhao, Wenbin,Zhang, Maoliang,&Ma, Lin.(2020).Coexisting Late Cenozoic Potassic and Sodic Basalts in NE China: Role of Recycled Oceanic Components in Intraplate Magmatism and Mantle Heterogeneity.LITHOSPHERE,2020(1),28.
MLA Lei, Ming,et al."Coexisting Late Cenozoic Potassic and Sodic Basalts in NE China: Role of Recycled Oceanic Components in Intraplate Magmatism and Mantle Heterogeneity".LITHOSPHERE 2020.1(2020):28.

入库方式: OAI收割

来源:地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。