中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Magma Origin and Evolution of Tengchong Cenozoic Volcanic Rocks from West Yunnan, China: Evidence from Whole Rock Geochemistry and Nd-Sr-Pb Isotopes

文献类型:期刊论文

作者Li Dapeng1; Luo Zhaohua1; Liu Jiaqi2; Chen Yuelong1; Jin Ye3
刊名ACTA GEOLOGICA SINICA-ENGLISH EDITION
出版日期2012-08-01
卷号86期号:4页码:867-878
关键词Cenozoic volcanism Nd-Sr-Pb isotopes geochemistry Tengchong
ISSN号1000-9515
DOI10.1111/j.1755-6724.2012.00712.x
文献子类Article
英文摘要Tengchong Cenozoic volcanics that have record key information on the tectonic evolution and mantle features of the southeast margin of the Tibetan Plateau are of great importance because of its unique eruption history spanning the entire Quaternary period. Magma origin and evolution of Tengchong Cenozoic volcanic rocks were studied on the basis of Nd-Sr-Pb isotope and major and trace element data from different eruptions in the Ma'anshan area. Different samples within one eruption show relative identical lithologies, chemical and isotopic compositions. However, the geochemical features for the five eruptions are distinct from each other. These volcanic rocks show low Mg# values (<45), moderate to high fractionation of LREEs and HREEs, and enrichment of Pb and Ba and depletion of Nb. Tengchong Cenozoic volcanic rocks were derived from an enriched mantle based on Nd-Sr-Pb isotopic studies. And lines of evidence show that crustal contamination should be involved before the eruption of different periods of Tengchong Cenozoic volcanic rocks. Older subducted components may be responsible for adakite recycling at various stages of evolution, which results in the origin of the enriched mantle source magma accounting for the isotopic features of Tengchong Cenozoic volcanic rocks. Segregated primitive magma pulsating injected into magma chamber, fractional crystallized and contaminated with crust component. Finally, magmas with distinct chemical and isotopic compositions for each eruption formed. The extension of the northeast segment of the Yingjiang tectonic belt triggered the pulsating eruption of the Cenozoic volcanics in the Tengchong area.
WOS关键词PROVINCE ; PETROGENESIS
WOS研究方向Geology
语种英语
WOS记录号WOS:000307378800007
出版者WILEY-BLACKWELL
资助机构Chinese Ministry of Science and Technology(Sinoprobe-05-03) ; Chinese Ministry of Science and Technology(Sinoprobe-05-03) ; Ministry of Education of China(20110022120003) ; Ministry of Education of China(20110022120003) ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; State Key Laboratory of Geological Processes and Mineral Resources(GPMR2011) ; State Key Laboratory of Geological Processes and Mineral Resources(GPMR2011) ; Chinese Ministry of Science and Technology(Sinoprobe-05-03) ; Chinese Ministry of Science and Technology(Sinoprobe-05-03) ; Ministry of Education of China(20110022120003) ; Ministry of Education of China(20110022120003) ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; State Key Laboratory of Geological Processes and Mineral Resources(GPMR2011) ; State Key Laboratory of Geological Processes and Mineral Resources(GPMR2011) ; Chinese Ministry of Science and Technology(Sinoprobe-05-03) ; Chinese Ministry of Science and Technology(Sinoprobe-05-03) ; Ministry of Education of China(20110022120003) ; Ministry of Education of China(20110022120003) ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; State Key Laboratory of Geological Processes and Mineral Resources(GPMR2011) ; State Key Laboratory of Geological Processes and Mineral Resources(GPMR2011) ; Chinese Ministry of Science and Technology(Sinoprobe-05-03) ; Chinese Ministry of Science and Technology(Sinoprobe-05-03) ; Ministry of Education of China(20110022120003) ; Ministry of Education of China(20110022120003) ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; State Key Laboratory of Geological Processes and Mineral Resources(GPMR2011) ; State Key Laboratory of Geological Processes and Mineral Resources(GPMR2011)
源URL[http://ir.iggcas.ac.cn/handle/132A11/84196]  
专题中国科学院地质与地球物理研究所
通讯作者Li Dapeng
作者单位1.China Univ Geosci, Sch Earth Sci & Resources, State Key Lab Geol Proc & Mineral Resources, Beijing 100083, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.China Univ Geosci, Sch Ocean Sci, Beijing 100083, Peoples R China
推荐引用方式
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Li Dapeng,Luo Zhaohua,Liu Jiaqi,et al. Magma Origin and Evolution of Tengchong Cenozoic Volcanic Rocks from West Yunnan, China: Evidence from Whole Rock Geochemistry and Nd-Sr-Pb Isotopes[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2012,86(4):867-878.
APA Li Dapeng,Luo Zhaohua,Liu Jiaqi,Chen Yuelong,&Jin Ye.(2012).Magma Origin and Evolution of Tengchong Cenozoic Volcanic Rocks from West Yunnan, China: Evidence from Whole Rock Geochemistry and Nd-Sr-Pb Isotopes.ACTA GEOLOGICA SINICA-ENGLISH EDITION,86(4),867-878.
MLA Li Dapeng,et al."Magma Origin and Evolution of Tengchong Cenozoic Volcanic Rocks from West Yunnan, China: Evidence from Whole Rock Geochemistry and Nd-Sr-Pb Isotopes".ACTA GEOLOGICA SINICA-ENGLISH EDITION 86.4(2012):867-878.

入库方式: OAI收割

来源:地质与地球物理研究所

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