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  4. 岩石圈演化国家重点实验室
Geochronology and geochemistry of Late Triassic.Early Jurassic granites in Moerdaoga area,NE China and its tectonic implications

文献类型：期刊论文

作者Li Yu1,2; Li WenQing2,3; Sun JinLong4
刊名ACTA PETROLOGICA SINICA
出版日期2022-10-01
卷号38期号:10页码:3021-3036
关键词Moerdaoga area Late Triassic-Early Jurassic Geochronology Geochemistry Southward subduction of the Mongol-Okhotsk Oceanic Plate
ISSN号1000-0569
英文摘要In this paper,we present new zircon U-Pb dating and whole.rock geochemical data for the granites in Moerdaoga area, NE China,with the aim of constraining its formation time,petrogenesis and the regional tectonic setting. Zircon grains from the granites in the study area are euhedral-subeuhedral in shape,and display fine-scale oscillatory growth zoning,indicating a magmatic origin. Zircon U-Pb dating indicates that two stages of Mesozoic magmatism are recorded in the Erguna Massif,namely during the Late Triassic (similar to 216Ma) and Early Jurassic (201 similar to 195Ma). The Late Triassic and Early Jurassic granites in the study area exhibit similar geochemical features. They contain high concentrations of SiO2 (67. 09% similar to 77. 05%)and Al2O3 (12. 18% similar to 16. 83%),and low concentrations of Fe2O3T (0. 11% similar to 0. 30%). They are classified as subalkaline,high-K calc-alkaline,metaluminous to peraluminous series,and exhibit chemical affinities to the I-type granites. In addition,the granites in the Moerdaoga area are enriched in light rare earth elements (LREEs)and large ion lithophile elements (LILEs),and depleted in heavy rare earth elements (HREEs)and high field strength elements (HFSEs). These features are similar to the igneous rocks that formed in the subduction zone. Additionally,the formation of coeval calc.alkaline rock associations in the Erguna Massif further indicated that the Late Triassic to Early Jurassic granites formed at an active continental margin setting. Combined with the temporal-spatial distributions of Mesozoic igneous in NE China,we concluded that the formation of the Late Triassic to Early Jurassic magmatism was related to the southward-s subduction of the Mongol. Okhotsk Oceanic Plate
WOS关键词ZHANGGUANGCAI RANGE MASSIF ; MESOZOIC INTRUSIVE ROCKS ; IN-SITU ANALYSIS ; U-PB AGES ; NE CHINA ; VOLCANIC-ROCKS ; NORTHEAST CHINA ; JIAMUSI MASSIF ; INNER-MONGOLIA ; TRACE-ELEMENTS
WOS研究方向Geology
语种英语
WOS记录号WOS:000905324300008
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/106842]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Li WenQing
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China
3.Minist Nat Resources, Key Lab Mineral Resources Evaluat Northeast Asia, Changchun 130061, Peoples R China
4.Hebei Bur Geol & Mineral Resources Explorat, Geol Brigade 8, Qinhuangdao 066000, Hebei, Peoples R China
推荐引用方式
GB/T 7714		 Li Yu,Li WenQing,Sun JinLong. Geochronology and geochemistry of Late Triassic.Early Jurassic granites in Moerdaoga area,NE China and its tectonic implications[J]. ACTA PETROLOGICA SINICA,2022,38(10):3021-3036.
APA Li Yu,Li WenQing,&Sun JinLong.(2022).Geochronology and geochemistry of Late Triassic.Early Jurassic granites in Moerdaoga area,NE China and its tectonic implications.ACTA PETROLOGICA SINICA,38(10),3021-3036.
MLA Li Yu,et al."Geochronology and geochemistry of Late Triassic.Early Jurassic granites in Moerdaoga area,NE China and its tectonic implications".ACTA PETROLOGICA SINICA 38.10(2022):3021-3036.

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来源：地质与地球物理研究所

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