Nature of three episodes of Paleoproterozoic magmatism (2180 Ma, 2115 Ma and 1890 Ma) in the Liaoji belt, North China with implications for tectonic evolution
文献类型:期刊论文
作者 | Wang, Xinping1,2; Peng, Peng1; Wang, Chong1,2; Yang, Shuyan1,2; Soderlund, Ulf3; Su, Xiangdong1,2 |
刊名 | PRECAMBRIAN RESEARCH
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出版日期 | 2017-09-01 |
卷号 | 298页码:252-267 |
关键词 | Eastern North China Craton Liaoji belt Paleoproterozoic Liaoji A-type granite Qingchengzi I-type granite Haicheng mafic sills |
ISSN号 | 0301-9268 |
DOI | 10.1016/j.precamres.2017.06.003 |
文献子类 | Article |
英文摘要 | Three episodes of Paleoproterozoic magmatism with distinctively different nature in the Liaoji belt of the Eastern North China Craton are discussed here: the 2200-2140 Ma Liaoji A-type granites, the 21602110 Ma Haicheng mafic sills and the similar to 1890 Ma Qingchengzi I-type granites. The Mafeng monzogranitic pluton, representative of the Liaoji A-type granites, gives a SIMS U-Pb zircon age of 2181 +/- 6 Ma (n = 20, MSWD = 4.3). The Qingchengzi plagiogranitic pluton, representative of the Qingchengzi I-type granites, gives a SIMS U-Pb zircon age of 1891 +/- 10 Ma (n = 8, MSWD = 1.8). The Mafeng monzogranites are high in Fe, Ti, K but low in Mg, Al and Ca. They have high abundance of total REEs (Sigma REE = 213-346 ppm). They are relatively depleted in feldspar-compatible elements (e.g., Eu and Sr) and HFSEs (e.g., Nb, Ta, P and Ti). They have high 10000 x Ga/Al ratios of 3.19-3.61 and Zr + Nb + Ce + Y concentrations of 472656 ppm, which are typical for A-type granite. The Qingchengzi plagiogranites have relatively high Al, Ca, Na but low Fe, Ti and K contents. They have low abundance of total REEs (Sigma REE = 17.6-21.6 ppm). They are enriched in LILEs (e.g., Ba, I< and Sr) but depleted in HFSEs (e.g., Nb, Ta, P, Ti and Y). These features, combined with extremely high Sr/Y ratios (327-413), are comparable with those of typical modern adakites. The Liaoji A-type granites show a source same to that of the Haicheng mafic sills and they originated from the Archean subcontinental lithospheric mantle plus with contamination from the Archean granites. However, the Qingchengzi I-type granites are interpreted to originate from subducted oceanic crust with significant contributions from sediments. The Liaoji A-type granites and the coeval bimodal volcanism in the Liaohe Group as well as the Haicheng mafic sills may represent episodic magmatism which was related to a protracted intra-continental rifting caused by lithospheric extension. The ca. 1890 Ma Qingchengzi I-type granites and coexisting S-type granites as well as the coeval regional metamorphism are favored to represent an active continental magmatism linked to Paleoproterozoic subduction. (C) 2017 Elsevier B.V. All rights reserved. |
WOS关键词 | A-TYPE GRANITES ; SOUTHERN JILIN PROVINCE ; WHOLE-ROCK GEOCHEMISTRY ; PB ZIRCON GEOCHRONOLOGY ; HF ISOTOPIC EVIDENCE ; U-PB ; JI BELT ; LIAONING PROVINCE ; CRUSTAL EVOLUTION ; EASTERN BLOCK |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000407654800016 |
出版者 | ELSEVIER SCIENCE BV |
资助机构 | Major State Research Development Project(2016YFC0600109) ; Major State Research Development Project(2016YFC0600109) ; CAS priority strategic program Linking the earth Interior Processes and Surface evolution (LIPS)(XDB18030205) ; CAS priority strategic program Linking the earth Interior Processes and Surface evolution (LIPS)(XDB18030205) ; National High-Level Talents Special Support Plan ; National High-Level Talents Special Support Plan ; Major State Research Development Project(2016YFC0600109) ; Major State Research Development Project(2016YFC0600109) ; CAS priority strategic program Linking the earth Interior Processes and Surface evolution (LIPS)(XDB18030205) ; CAS priority strategic program Linking the earth Interior Processes and Surface evolution (LIPS)(XDB18030205) ; National High-Level Talents Special Support Plan ; National High-Level Talents Special Support Plan ; Major State Research Development Project(2016YFC0600109) ; Major State Research Development Project(2016YFC0600109) ; CAS priority strategic program Linking the earth Interior Processes and Surface evolution (LIPS)(XDB18030205) ; CAS priority strategic program Linking the earth Interior Processes and Surface evolution (LIPS)(XDB18030205) ; National High-Level Talents Special Support Plan ; National High-Level Talents Special Support Plan ; Major State Research Development Project(2016YFC0600109) ; Major State Research Development Project(2016YFC0600109) ; CAS priority strategic program Linking the earth Interior Processes and Surface evolution (LIPS)(XDB18030205) ; CAS priority strategic program Linking the earth Interior Processes and Surface evolution (LIPS)(XDB18030205) ; National High-Level Talents Special Support Plan ; National High-Level Talents Special Support Plan |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/61846] ![]() |
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 | Peng, Peng |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China 3.Lund Univ, Dept Geol, S-22362 Lund, Sweden |
推荐引用方式 GB/T 7714 | Wang, Xinping,Peng, Peng,Wang, Chong,et al. Nature of three episodes of Paleoproterozoic magmatism (2180 Ma, 2115 Ma and 1890 Ma) in the Liaoji belt, North China with implications for tectonic evolution[J]. PRECAMBRIAN RESEARCH,2017,298:252-267. |
APA | Wang, Xinping,Peng, Peng,Wang, Chong,Yang, Shuyan,Soderlund, Ulf,&Su, Xiangdong.(2017).Nature of three episodes of Paleoproterozoic magmatism (2180 Ma, 2115 Ma and 1890 Ma) in the Liaoji belt, North China with implications for tectonic evolution.PRECAMBRIAN RESEARCH,298,252-267. |
MLA | Wang, Xinping,et al."Nature of three episodes of Paleoproterozoic magmatism (2180 Ma, 2115 Ma and 1890 Ma) in the Liaoji belt, North China with implications for tectonic evolution".PRECAMBRIAN RESEARCH 298(2017):252-267. |
入库方式: OAI收割
来源:地质与地球物理研究所
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