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
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出版日期 | 2020-06-01 |
卷号 | 2020期号:1页码:28 |
ISSN号 | 1941-8264 |
DOI | 10.2113/2020/8875012 |
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
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