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  2. 地质与地球物理研究所
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  4. 中国科学院新生代地质与环境重点实验室
Geochemical constraints on the origin of late Cenozoic basalts in the Mt. Changbai volcanic field, NE China: evidence for crustal recycling

文献类型：期刊论文

作者Lei, Ming2,3,4; Guo, Zhengfu2,3,4; Sun, Yutao1; Zhang, Maoliang2,3,4; Zhang, Lihong2,3,4; Ma, Lin2,3,4
刊名INTERNATIONAL GEOLOGY REVIEW
出版日期2019-11-11
页码21
关键词Peridotite pyroxenite enriched mantle mantle transition zone Mt Changbai basalts NE China
ISSN号0020-6814
DOI10.1080/00206814.2019.1686660
英文摘要We conducted a systematic geochemical study of the Mt. Changbai basalts (MCBs) in NE China to better constrain their mantle sources and petrogenesis. The MCBs display ocean island basalt-like trace element patterns (e.g., positive Nb-Ta anomalies) and variable MgO contents (3.2-10.0 wt.%), trace element ratios (e.g., Ba/Nb and Rb/Nb), and Sr-Nd-Pb-Hf isotopic ratios (Sr-87/Sr-86((i)) = 0.704497-0.705629; epsilon Nd-(i) = - 2.8 to +3.3; Pb-206/Pb-204((i)) = 16.9-18.1; epsilon Hf = -1.2 to +6.2), which indicate derivation from a heterogeneous mantle source. The least evolved samples (MgO > 7 wt.%), with moderate Fe/Mn and FC3MS (defined as FeOT/CaO - 3MgO/SiO2) values, require a hybrid pyroxenite-peridotite mantle source. The isotopic compositions indicate the mantle source is a mixture between depleted mid-ocean ridge basalt mantle and two enriched mantle components. Our geochemical and published geophysical data indicate that these two enriched components are recycled ancient sediments and Pacific oceanic crust, which were derived from the mantle transition zone. An upwelling wet plume from the mantle transition zone transported these two enriched components into the asthenospheric mantle. These enriched components were then transformed into pyroxenite and/or eclogite through melt-rock reaction or mechanical mixing with asthenospheric mantle peridotite. We further propose that partial melting of this heterogeneous asthenospheric mantle containing fusible pyroxenite and/or eclogite (i.e., the enriched components) and refractory peridotite produced the MCBs.
WOS关键词LITHOSPHERIC MANTLE BENEATH ; PARTIAL MELTING EXPERIMENTS ; TRANSITION-ZONE ; TRACE-ELEMENT ; NORTH CHINA ; OCEANIC-CRUST ; EASTERN CHINA ; POTASSIC BASALTS ; STAGNANT SLAB ; MAJOR-ELEMENT
资助项目Natural Science Foundation of China[41702361] ; Natural Science Foundation of China[41572321] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDB26000000] ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences[QYZDY-SSW-DQC030]
WOS研究方向Geology
语种英语
WOS记录号WOS:000495524200001
出版者TAYLOR & FRANCIS INC
资助机构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 Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of 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 Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of 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 Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of 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 Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences ; Key Research Project of Frontier Sciences of Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/95765]  
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.Hebei GEO Univ, Coll Resources, Shijiazhuang, Hebei, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, POB 9825, Beijing 100029, Peoples R China
3.CAS Ctr Excellence Life & Paleoenvironm, Beijing, Peoples R China
4.Univ Chinese Acad Sci, Beijing, Peoples R China
推荐引用方式
GB/T 7714		 Lei, Ming,Guo, Zhengfu,Sun, Yutao,et al. Geochemical constraints on the origin of late Cenozoic basalts in the Mt. Changbai volcanic field, NE China: evidence for crustal recycling[J]. INTERNATIONAL GEOLOGY REVIEW,2019:21.
APA Lei, Ming,Guo, Zhengfu,Sun, Yutao,Zhang, Maoliang,Zhang, Lihong,&Ma, Lin.(2019).Geochemical constraints on the origin of late Cenozoic basalts in the Mt. Changbai volcanic field, NE China: evidence for crustal recycling.INTERNATIONAL GEOLOGY REVIEW,21.
MLA Lei, Ming,et al."Geochemical constraints on the origin of late Cenozoic basalts in the Mt. Changbai volcanic field, NE China: evidence for crustal recycling".INTERNATIONAL GEOLOGY REVIEW (2019):21.

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来源：地质与地球物理研究所

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