中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Hf isotopic mapping of the Paleozoic-Mesozoic granitoids from the Jiamusi and Songnen blocks, NE China: Implications for their tectonic division and juvenile continental crustal growth

文献类型:期刊论文

作者Ge, Mao-Hui4; Li, Long1; Wang, Tao4; Zhang, Jin-Jiang2; Tong, Ying4; Guo, Lei4; Liu, Kai3; Feng, Lin2; Song, Peng4; Yuan, Jian-Guo4
刊名LITHOS
出版日期2021-04-01
卷号386页码:15
关键词Granitoids Hf isotopic mapping Crustal growth Northeast China Central Asian Orogenic Belt
ISSN号0024-4937
DOI10.1016/j.lithos.2021.106048
英文摘要The long-standing controversies in tectonic boundary, the nature of basement rocks, and the Phanerozoic continental crustal growth in the eastern Central Asian Orogenic Belt (CAOB) inNE China have been the key barriers in the understanding of the regional tectonic evolution. In this paper, we integrated published and new zircon U-Pb and Hf isotopic data of the Phanerozoic granitoids from the Jiamusi Block and the Lesser Xing'an-Zhangguangcai Range (LXZR) for a zircon Hf isotopicmapping of the region. Themapping results outlined three Hf isotopic provinces on the basis of TDMC ages: Province I (TDMC = 2.0-1.6 Ga, eHf(t) = -7.0 to -5.2) and Province II (TDMC = 1.6-1.1 Ga, eHf(t) = -4.6 to +3.9) represent the ancient basements in the Jiamusi Block; Province III (TDMC = 1.1-0.4 Ga with eHf(t) = +2.1 to +13.1) represents the juvenile crustal components in the LXZR. Province I (total area - 6000 km2) is sporadically exposedwithin Province II (-121,000 km2); the latter is bounded to Province III (-144,000 km2) along a sharp SE-NWboundary -130 kmwest of theMudanjiang Fault. This suggests that at least the part of the Songnen Block to the east of this boundary was in the same tectonic unit with the Jiamusi Block in the Paleozoic. Province III spatially accounts for about 53% of the study area, indicating a significant Mesozoic growth of continental crustal in the easternmost CAOB.
资助项目National Key Research and Development Project of China[2017YFC0601301] ; NSFC[41902240] ; NSFC[41730210]
WOS研究方向Geochemistry & Geophysics ; Mineralogy
语种英语
WOS记录号WOS:000632736400001
出版者ELSEVIER
资助机构National Key Research and Development Project of China ; National Key Research and Development Project of China ; NSFC ; NSFC ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; NSFC ; NSFC ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; NSFC ; NSFC ; National Key Research and Development Project of China ; National Key Research and Development Project of China ; NSFC ; NSFC
源URL[http://ir.iggcas.ac.cn/handle/132A11/101048]  
专题中国科学院地质与地球物理研究所
通讯作者Ge, Mao-Hui
作者单位1.Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2E3, Canada
2.Peking Univ, Sch Earth & Space Sci, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
4.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China
推荐引用方式
GB/T 7714
Ge, Mao-Hui,Li, Long,Wang, Tao,et al. Hf isotopic mapping of the Paleozoic-Mesozoic granitoids from the Jiamusi and Songnen blocks, NE China: Implications for their tectonic division and juvenile continental crustal growth[J]. LITHOS,2021,386:15.
APA Ge, Mao-Hui.,Li, Long.,Wang, Tao.,Zhang, Jin-Jiang.,Tong, Ying.,...&Yuan, Jian-Guo.(2021).Hf isotopic mapping of the Paleozoic-Mesozoic granitoids from the Jiamusi and Songnen blocks, NE China: Implications for their tectonic division and juvenile continental crustal growth.LITHOS,386,15.
MLA Ge, Mao-Hui,et al."Hf isotopic mapping of the Paleozoic-Mesozoic granitoids from the Jiamusi and Songnen blocks, NE China: Implications for their tectonic division and juvenile continental crustal growth".LITHOS 386(2021):15.

入库方式: OAI收割

来源:地质与地球物理研究所

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