Eastward Asthenospheric Flow From NE Tibet Inferred by Joint Inversion of Teleseismic Body and Surface Waves: Insight Into Widespread Continental Deformation in Eastern China
文献类型:期刊论文
作者 | Guo, Zhen4,5,6; Li, Shilin6; Yu, Yong5,6; Chen, Y. John5,6; Yang, Yingjie3; Xu, Bo2; Liang, Xiaofeng1 |
刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH |
出版日期 | 2022-08-01 |
卷号 | 127期号:8页码:18 |
ISSN号 | 2169-9313 |
关键词 | joint inversion lateral asthenospheric flow Ordos block craton reworking intraplate volcanism Qinling belt |
DOI | 10.1029/2022JB024410 |
英文摘要 | During the last 50 Ma, the eastern Eurasian continent has experienced widespread crustal and lithospheric deformation. However, mechanisms in creating such widespread intra-continental deformation are still not well understood. Here, we present a 3-D S-wave velocity model of the northeastern Tibetan Plateau and adjacent regions by jointly inverting teleseismic body and surface waves. The resulting model clearly suggests that lateral extrusion of asthenosphere from northern Tibet is being blocked by the thick cratonic keels of Ordos and Sichuan, and therefore the asthenosphere is channeled into a strong eastward flow beneath the northern Qinglin between these two cratonic keels. Our results also demonstrate that continental deformation in eastern Eurasia is likely influenced by the small-scale convection when the lateral asthenospheric flow from NE Tibet encounters preexisting continental lithospheric steps to the east of Ordos. |
WOS关键词 | INTRAPLATE VOLCANISM ; RECEIVER FUNCTION ; TRAVEL-TIMES ; MANTLE ; BENEATH ; PHASE ; ASIA ; PLATEAU ; CRATON ; CONVERGENCE |
资助项目 | NSFC[42122027] ; NSFC[41974052] ; NSFC[U1901602] ; NSFC[42074067] ; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)[GML2019ZD0210] |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
出版者 | AMER GEOPHYSICAL UNION |
WOS记录号 | WOS:000837056300001 |
资助机构 | NSFC ; NSFC ; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; NSFC ; NSFC ; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; NSFC ; NSFC ; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; NSFC ; NSFC ; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) ; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/108458] |
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 | Guo, Zhen |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China 2.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing, Peoples R China 3.Southern Univ Sci & Technol, Dept Earth & Space Sci, Shenzhen, Peoples R China 4.Shanghai Sheshan Natl Geophys Observ & Res Stn, Shanghai, Peoples R China 5.Shenzhen Branch Southern Marine Sci & Engn Guangd, Shenzhen, Peoples R China 6.Southern Univ Sci & Technol, Dept Ocean Sci & Engn, Shenzhen, Peoples R China |
推荐引用方式 GB/T 7714 | Guo, Zhen,Li, Shilin,Yu, Yong,et al. Eastward Asthenospheric Flow From NE Tibet Inferred by Joint Inversion of Teleseismic Body and Surface Waves: Insight Into Widespread Continental Deformation in Eastern China[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2022,127(8):18. |
APA | Guo, Zhen.,Li, Shilin.,Yu, Yong.,Chen, Y. John.,Yang, Yingjie.,...&Liang, Xiaofeng.(2022).Eastward Asthenospheric Flow From NE Tibet Inferred by Joint Inversion of Teleseismic Body and Surface Waves: Insight Into Widespread Continental Deformation in Eastern China.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,127(8),18. |
MLA | Guo, Zhen,et al."Eastward Asthenospheric Flow From NE Tibet Inferred by Joint Inversion of Teleseismic Body and Surface Waves: Insight Into Widespread Continental Deformation in Eastern China".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 127.8(2022):18. |
入库方式: OAI收割
来源:地质与地球物理研究所
浏览0
下载0
收藏0
其他版本
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。