中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Petrogenesis and tectonic implication of the Late Mesozoic volcanic rocks in East Mongolia

文献类型:期刊论文

作者Bars, Amarjargal1,3; Miao, Laicheng1,2; Fochin, Zhang1,2; Baatar, Munkhtsengel4; Anaad, Chimedtseren4; Togtokh, Khasmaral1,3
刊名GEOLOGICAL JOURNAL
出版日期2018-11-01
卷号53期号:6页码:2449-2470
关键词East Mongolia Late Mesozoic volcanic rock Mongol-Okhotsk suture Paleo-Pacific subduction
ISSN号0072-1050
DOI10.1002/gj.3080
英文摘要This paper presents new geochemical and geochronological data of the Late Mesozoic volcanic rocks in East Mongolia. These volcanic rocks belong to high-K calc-alkaline and shoshonitic series and exhibit features of bimodal rocks. The mafic rocks have elevated incompatible trace element concentrations and significantly negative Nb, Ta, and Ti anomalies, with Sr-87/Sr-86(i) and Nd-&(t) values of 0.70502-0.70572 and -1.72459 to +1.720736, respectively, which suggest that the mafic magma was derived from a lithospheric mantle source that might have been metasomatized by subduction-derived fluids, experienced fractional crystallization, and was contaminated by crustal materials. The felsic rocks have similar rare earth element patterns to the mafic rocks but show much more significantly negative Eu and Sr anomalies. The felsic rocks have higher Sr-87/Sr-86(i) values of 0.706496-0.71104 than the mafic rocks but similar Nd-&(t) values (-0.28003 to +2.928506) to the mafic ones. These data indicate that the felsic rocks originated from partial melting of a crustal source that is dominated by juvenile mafic rocks. Our new K-Ar dating, together with previous data, shows that the Late Mesozoic volcanism in East Mongolia took place during the Late Jurassic-Early Cretaceous between ca. 155 and 99 Ma. The model of back-arc extension, possibly induced by slab rollback of the westward subducted Pacific Plate and the subduction zone retreat, can explain the geodynamic setting and the eastward younging trend of the Late Mesozoic volcanism in East Mongolia and in adjacent NE China.
WOS关键词GREAT XINGAN RANGE ; U-PB AGES ; NE CHINA CONSTRAINTS ; DA-HINGGAN MOUNTAINS ; LITHOSPHERIC EXTENSION ; INNER-MONGOLIA ; CRUSTAL GROWTH ; OROGENIC BELT ; OKHOTSK OCEAN ; SIKHOTE-ALIN
资助项目National Key R&D Program of China[2017YFC0601306] ; National Natural Science Foundation of China[41772230] ; National Natural Science Foundation of China[41702217] ; National Natural Science Foundation of China[41502217] ; Ministry of Science and Technology of China[2012FY120100]
WOS研究方向Geology
语种英语
WOS记录号WOS:000450653800004
出版者WILEY
资助机构National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China ; Ministry of Science and Technology of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/89615]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Miao, Laicheng
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Mongolian Univ Sci & Technol, Sch Geol & Min, Ulaanbaatar 14191, Mongol Peo Rep
推荐引用方式
GB/T 7714
Bars, Amarjargal,Miao, Laicheng,Fochin, Zhang,et al. Petrogenesis and tectonic implication of the Late Mesozoic volcanic rocks in East Mongolia[J]. GEOLOGICAL JOURNAL,2018,53(6):2449-2470.
APA Bars, Amarjargal,Miao, Laicheng,Fochin, Zhang,Baatar, Munkhtsengel,Anaad, Chimedtseren,&Togtokh, Khasmaral.(2018).Petrogenesis and tectonic implication of the Late Mesozoic volcanic rocks in East Mongolia.GEOLOGICAL JOURNAL,53(6),2449-2470.
MLA Bars, Amarjargal,et al."Petrogenesis and tectonic implication of the Late Mesozoic volcanic rocks in East Mongolia".GEOLOGICAL JOURNAL 53.6(2018):2449-2470.

入库方式: OAI收割

来源:地质与地球物理研究所

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