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  4. 岩石圈演化国家重点实验室
Accretion, subduction erosion, and tectonic extrusion during late Paleozoic to Mesozoic orogenesis in NE China

文献类型：期刊论文

作者Aouizerat, Arthur11; Xiao, Wenjiao1,10,11; Schulmann, Karel7,8,9; Windley, Brian F.6; Zhou, Jianbo5; Zhang, Jinjiang3,4; Ao, Songjian10,11; Song, Dongfang10,11; Monie, Patrick2; Liu, Kai11
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2020-06-01
卷号194页码:48
关键词Accretionary complex Subduction erosion Tectonic extrusion Heilongjiang complex NE China
ISSN号1367-9120
DOI10.1016/j.jseaes.2020.104258
英文摘要The high-pressure Heilongjiang Complex records a long and complicated evolution from the late Paleozoic to Mesozoic in NE China, which is still subject to controversy. In this paper we present a new detailed study including structural, geochemical and geochronological analyses (Ar-Ar dating on metamorphic minerals, U-Pb SIMS dating on zircons). Two main periods of oceanward accretionary growth are identified between 305 Ma and 195 Ma and around 112-101 Ma. These periods of accretionary growth were associated with the emplacement of voluminous magmatism, slab roll-back with continental back-arc extension, and growth of a forearc accretionary prism. Between these periods of accretionary growth, a major phase of regional subduction erosion took place between 195 Ma and 142 Ma at the eastern edge of the Songliao Block. The main effects of this subduction erosion phase were that regional Jurassic-early Cretaceous extrusion overlapped with Mesozoic accretion and erosion in NE China, which disturbed the initial orogenic architecture. With a review of relevant zircon ages of this accretionary orogen, we unravel the complicated geodynamic history of accretion, subduction erosion and tectonic extrusion that shaped NE China from the late Paleozoic to Mesozoic.
WOS关键词ZIRCON U-PB ; ZHANGGUANGCAI RANGE MASSIF ; EASTERN JIAMUSI MASSIF ; BIMODAL IGNEOUS ROCKS ; PACIFIC-TYPE OROGENY ; HEILONGJIANG COMPLEX ; NORTHEASTERN CHINA ; VOLCANIC-ROCKS ; HF ISOTOPES ; MUDANJIANG OCEAN
资助项目National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41730210] ; National Key Research and Development Program of China[2017YFC0601201] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB18020203] ; Key Research Program of Frontier Sciences, CAS[QYZDJ-SSW-SYS012]
WOS研究方向Geology
语种英语
WOS记录号WOS:000538820400001
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS ; Key Research Program of Frontier Sciences, CAS
源URL[http://ir.iggcas.ac.cn/handle/132A11/96889]  
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Xiao, Wenjiao
作者单位1.Chinese Acad Sci, Xinjiang Res Ctr Mineral Resources, Xinjiang Inst Ecol & Geog, Urumqi 830011, Peoples R China
2.Univ Montpellier, Geosci Montpellier UMR CNRS 5243, Montpellier, France
3.Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
4.Minist Educ, Key Lab Orogen Belts & Crustal Evolut, Beijing, Peoples R China
5.Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China
6.Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England
7.Czech Geol Survey, Ctr Lithospher Res, Klarov 3, Prague, Czech Republic
8.Univ Strasbourg, Strasbourg, France
9.CNRS, Inst Phys Globe Strasbourg, IPGS UMR 7516, Strasbourg, France
10.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714		 Aouizerat, Arthur,Xiao, Wenjiao,Schulmann, Karel,et al. Accretion, subduction erosion, and tectonic extrusion during late Paleozoic to Mesozoic orogenesis in NE China[J]. JOURNAL OF ASIAN EARTH SCIENCES,2020,194:48.
APA Aouizerat, Arthur.,Xiao, Wenjiao.,Schulmann, Karel.,Windley, Brian F..,Zhou, Jianbo.,...&Liu, Kai.(2020).Accretion, subduction erosion, and tectonic extrusion during late Paleozoic to Mesozoic orogenesis in NE China.JOURNAL OF ASIAN EARTH SCIENCES,194,48.
MLA Aouizerat, Arthur,et al."Accretion, subduction erosion, and tectonic extrusion during late Paleozoic to Mesozoic orogenesis in NE China".JOURNAL OF ASIAN EARTH SCIENCES 194(2020):48.

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来源：地质与地球物理研究所

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