A craton-like subcontinental lithospheric mantle beneath the Trans-North China Orogen revealed by the ca. 1.54?Ga kimberlites
文献类型：期刊论文
| 作者 | Zhu, Yu-Sheng2,4; Yang, Jin-Hui1,3; Li, Qiu-Li1,3; Wang, Hao3 ; Wu, Ya-Dong3; Wu, Fu-Yuan1,3
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| 刊名 | TERRA NOVA
 |
| 出版日期 | 2023-09-21 |
| 页码 | 7 |
| 关键词 | baddeleyite kimberlite lithospheric mantle NCC olivine |
| ISSN号 | 0954-4879 |
| DOI | 10.1111/ter.12683 |
| 英文摘要 | Ancient orogens within the supercontinent like Columbia can remain stable evolution as long as the cratons. What kind of lithospheric mantle was beneath those orogens and how it evolved into a stable state are still enigmatic. The Trans-North China orogen (TNCO) is one of the typical collisional orogens within the Columbia supercontinent and was formed at ca. 1.85 Ga. Our work reveals that a cluster of kimberlites intruded the orogenic belt at ca. 1.54 Ga. These rocks were originally generated under a thick lithosphere (>200 km). Their entrained olivine cores show a composition of overlapping olivines from refractory mantle peridotites. The results suggest a thick and refractory lithospheric mantle beneath the TNCO at ca. 1.54 Ga. Such craton-like property may result from large volume melt extraction from the lithospheric mantle, possibly caused by the ca. 1.78 Ga large igneous event, which eventually induces the long-term stability of the TNCO during the subsequent supercontinent cycle. |
| WOS关键词 | SINO-KOREAN CRATON ; U-PB SYSTEMATICS ; HF ISOTOPES ; OFF-CRATON ; BADDELEYITE ; GEOCHEMISTRY ; PETROGENESIS ; CONSTRAINTS ; INHERITANCE ; XENOLITHS |
| 资助项目 | We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation[42288201] ; National Natural Science Foundation of China[2016YFC0600109] ; National Key Ramp;amp;D Program of China |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:001069254000001 |
| 出版者 | WILEY |
| 资助机构 | We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; 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 Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; 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 Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; 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 Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; We thank Yu Liu, Xiao-Xiao Ling, Jiao Li and Li-Hui Jia for helping with the analysis. We also thank two anonymous reviewers for their constructive comments and Jason Morgan for help and handling our paper. This study was supported by funds from the Nation ; 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 Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China ; National Key Ramp;amp;D Program of China |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/110859]  |
| 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 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 | Zhu, Yu-Sheng |
| 作者单位 | 1.Univ Chinese Acad Sci, Key Lab Computat Geodynam, Beijing, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhu, Yu-Sheng,Yang, Jin-Hui,Li, Qiu-Li,et al. A craton-like subcontinental lithospheric mantle beneath the Trans-North China Orogen revealed by the ca. 1.54?Ga kimberlites[J]. TERRA NOVA,2023:7. |
| APA | Zhu, Yu-Sheng,Yang, Jin-Hui,Li, Qiu-Li,Wang, Hao,Wu, Ya-Dong,&Wu, Fu-Yuan.(2023).A craton-like subcontinental lithospheric mantle beneath the Trans-North China Orogen revealed by the ca. 1.54?Ga kimberlites.TERRA NOVA,7. |
| MLA | Zhu, Yu-Sheng,et al."A craton-like subcontinental lithospheric mantle beneath the Trans-North China Orogen revealed by the ca. 1.54?Ga kimberlites".TERRA NOVA (2023):7. |
入库方式： OAI收割
来源：地质与地球物理研究所
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