中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Carboniferous magmatic records of central Mongolia and its implications for the southward subduction of the Mongol-Okhotsk Ocean

文献类型:期刊论文

作者Zhu, Mingshuai4,5; Miao, Laicheng4,5; Zhang, Fuqin4,5; Ganbat, Ariuntsetseg1,2; Baatar, Munkhtsengel1,2; Anaad, Chimedtseren1,2; Yang, Shunhu4,5; Wang, Zeli3
刊名INTERNATIONAL GEOLOGY REVIEW
出版日期2022-05-19
页码20
关键词Mongol-Okhotsk Ocean carboniferous southward subduction continental collision
ISSN号0020-6814
DOI10.1080/00206814.2022.2076161
英文摘要The now-extinct Palaeozoic to Mesozoic Mongol-Okhotsk Ocean is evidenced by the Mongol-Okhotsk suture, which stretches from central Mongolia to the Sea of Okhotsk. The geodynamics of southward subduction of the Mongol-Okhotsk Ocean remain enigmatic, especially whether the subduction began during the Carboniferous is highly debated. In this paper we present new zircon U-Pb ages and whole-rock geochemical data for the Carboniferous magmatic rocks in Northeast Mongolia. Zircon U-Pb dating indicates that the Adaatsag dacite, Northern Bayanjargalan gabbro-diorite and Bagannur pluton were emplaced at ca. 325 Ma, ca. 316 Ma, and ca. 305 Ma, respectively. Occurrences of these rocks together constitute a Carboniferous magmatic belt to the northwest of the Middle Gobi volcanic-plutonic belt. The ages of trapped zircon xenocrysts within the Bagannur pluton indicate that the basement of this magmatic belt is the Ereendavaa terrane. Geochemical analysis indicates that these magmatic rocks were formed in an Andean-type active margin, which provides robust evidence for southward subduction of the Mongol-Okhotsk Ocean during the Late Carboniferous. By combining all the available data, we argue that the onset of the Central Mongolia-Tsagaan Uul continental collision during the Late Carboniferous - Early Permian may have triggered the beginning of an active margin of the Mongol-Okhotsk Ocean along the northern coast of the Central Mongolia microcontinent.
WOS关键词U-PB AGES ; ASIAN OROGENIC BELT ; TECTONIC EVOLUTION ; VOLCANIC-ROCKS ; ERGUNA MASSIF ; IGNEOUS ROCKS ; NORTHEASTERN MONGOLIA ; CONTINENTAL-CRUST ; CALC-ALKALINE ; ZIRCON
资助项目Strategic Priority Research Program of Chinese Academy of Sciences[XDB 41000000] ; National Natural Science Foundation of China[41772230] ; Chinese Academy of Sciences[GJHZ1805]
WOS研究方向Geology
语种英语
WOS记录号WOS:000797390500001
出版者TAYLOR & FRANCIS INC
资助机构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 ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; 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 ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; 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 ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; 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 ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/105945]  
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Zhu, Mingshuai
作者单位1.Univ Hong Kong, Div Earth & Planetary Sci, Pokfulam Rd, Hong Kong, Peoples R China
2.Univ Hong Kong, Lab Space Res, Pokfulam Rd, Hong Kong, Peoples R China
3.Shandong Univ Sci & Technol, Shandong Key Lab Deposit Mineralizat & Sedimentar, Qingdao, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
5.Chinese Acad Sci, Inst Earth Sci, Beijing, Peoples R China
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Zhu, Mingshuai,Miao, Laicheng,Zhang, Fuqin,et al. Carboniferous magmatic records of central Mongolia and its implications for the southward subduction of the Mongol-Okhotsk Ocean[J]. INTERNATIONAL GEOLOGY REVIEW,2022:20.
APA Zhu, Mingshuai.,Miao, Laicheng.,Zhang, Fuqin.,Ganbat, Ariuntsetseg.,Baatar, Munkhtsengel.,...&Wang, Zeli.(2022).Carboniferous magmatic records of central Mongolia and its implications for the southward subduction of the Mongol-Okhotsk Ocean.INTERNATIONAL GEOLOGY REVIEW,20.
MLA Zhu, Mingshuai,et al."Carboniferous magmatic records of central Mongolia and its implications for the southward subduction of the Mongol-Okhotsk Ocean".INTERNATIONAL GEOLOGY REVIEW (2022):20.

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来源:地质与地球物理研究所

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