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| DOI | 10.1111/ter.12714 |
| Crustal anisotropy beneath southeast Tibet revealed by Pms arrival times | |
| 发表日期 | 2024 |
| ISSN | 0954-4879 |
| EISSN | 1365-3121 |
| 英文摘要 | The mechanisms of uplift and deformation of the Tibetan Plateau are highly concerned. Understanding the crustal deformation mechanisms beneath southeast Tibet is important as it is located at the major path of Tibet's growth or expansion. Recent studies are controversial on whether large-scale crustal flow is dominant or not in this area. We applied Pms arrival time technique based on receiver function to events from 10 years of observation and obtained the crustal anisotropy parameters. The results show that both the large-scale faults and local crustal flow play major roles in crustal deformation in interested areas, while the large-scale crustal flow is not very well preferred. Furthermore, the crustal anisotropy in southeast of the study area is characterized by complex anisotropies, which may be potentially related to the converging of two mantle flows from various origins. |
| 英文关键词 | crustal anisotropy; local crustal flow; Pms arrival times; southeast Tibet |
| 语种 | 英语 |
| WOS研究方向 | Geology |
| WOS类目 | Geosciences, Multidisciplinary |
| WOS记录号 | WOS:001198621400001 |
| 来源期刊 | TERRA NOVA
 |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/285922 |
| 作者单位 | Chinese Academy of Sciences; Institute of Geology & Geophysics, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; China Earthquake Administration; Institute of Earthquake Forecasting, CEA |
| 推荐引用方式 GB/T 7714 | . Crustal anisotropy beneath southeast Tibet revealed by Pms arrival times[J],2024. |
| APA | (2024).Crustal anisotropy beneath southeast Tibet revealed by Pms arrival times.TERRA NOVA. |
| MLA | "Crustal anisotropy beneath southeast Tibet revealed by Pms arrival times".TERRA NOVA (2024). |
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