A review of recent earthquake-induced landslides on the Tibetan Plateau

B Zhao, L Su, Q Xu, W Li, C Xu, Y Wang - Earth-Science Reviews, 2023 - Elsevier
Earthquake-induced landslides, also called seismic landslides (SLs), are some of the most
catastrophic natural hazards on the Tibetan Plateau (TP). They have frequently caused …

[HTML][HTML] 芦山4.20 地震破裂过程及其致灾特征初步分析

张勇, 许力生, 陈运泰 - 地球物理学报, 2013 - data.geophy.cn
采用全球地震台网的远震地震波数据快速反演了2013 年4 月20 日雅安芦山地震(芦山4.20
地震) 的破裂过程, 在震后3 小时得到并发布了相关测定结果. 结果显示这次地震的震级约MW …

[PDF][PDF] 2014 年云南鲁甸犕犠6.1 地震: 一次共轭破裂地震

张勇, 陈运泰, 许力生, 魏星, 金明培, 张森 - 地球物理学报, 2015 - dsjyj.com.cn
摘要烈度与余震分布显示2014 年云南鲁甸犕W6. 1 (犕S6. 5) 地震的发震构造较复杂.
为深入了解鲁甸地震的发震断层与破裂特征, 本文考虑了单一断层破裂和共轭断层破裂的情况 …

[HTML][HTML] Coulomb stress changes associated with the M7. 3 Maduo earthquake and implications for seismic hazards

Y Li, L Huang, R Ding, S Yang, L Liu, S Zhang… - Natural Hazards …, 2021 - Elsevier
Abstract On May 21, 2021, the M7. 3 Maduo earthquake occurred within the Bayan Har
Block, one of the most seismically active regions in the Tibetan Plateau. This aroused …

Rupture process of the Lushan 4.20 earthquake and preliminary analysis on the disaster-causing mechanism

Y Zhang, LS XU, YT CHEN - Chinese Journal of Geophysics, 2013 - en.dzkx.org
Fast inversion for the rupturing process of the 20 April 2013 Lushan, Ya'an earthquake was
conducted about 3 hours after the earthquake occurrence by using the GSN teleseismic …

[HTML][HTML] 2021年3月19日那曲M6.1地震震源区应力应变特征及其动力学意义

李玉江, 邵志刚, 胡幸平, 石富强, 刘皓晴, 陈连旺 - 地球物理学报, 2022 - dsjyj.com.cn
2021 年3 月19 日在西藏那曲发生M6. 1 地震, 震源区应力应变环境与应力演化对于理解该地震
的孕育背景与发震机制具有重要的意义. 地震发生后, 快速收集震中周边的实测应力数据 …

Rupture process of the M s7.0 Lushan earthquake, 2013

CL Liu, Y Zheng, C Ge, X Xiong, HT Hsu - Science China Earth Sciences, 2013 - Springer
Abstract On April 20, 2013 at 8: 02 am, a magnitude 7.0 earthquake occurred in Lushan
County, Sichuan Province, China, which induces massive landslides, causes great losses to …

[PDF][PDF] 利用区域宽频带数据反演鲁甸犕犛6.5 级地震震源破裂过程

刘成利, 郑勇, 熊熊, 付芮, 单斌, 刁法启 - 地球物理学报, 2014 - dsjyj.com.cn
摘要基于有限断层模型反演方法, 我们利用区域宽频带数据反演得到了2014 年8 月3
日鲁甸犕S6. 5 级地震的震源破裂过程. 反演结果显示: 此次地震的发震断层走向为北北西向 …

[HTML][HTML] 1900 年以来巴颜喀拉块体应力演化与周缘强震关系的数值模拟研究

李平恩, 廖力, 奉建州, 刘盼 - 地球物理学报, 2019 - html.rhhz.net
以巴颜喀拉块体为研究对象, 考虑区域地质构造差异, 主要活动断裂带, 活动块体和边界断裂带的
划分结果, 引入深部三维速度结构, 建立能反映地表起伏和岩石圈分层结构的青藏高原地区三维 …

Source characteristics of the 2015 MW 7.8 Gorkha (Nepal) earthquake and its MW 7.2 aftershock from space geodesy

W Feng, E Lindsey, S Barbot, S Samsonov, K Dai, P Li… - Tectonophysics, 2017 - Elsevier
Abstract On April 25, 2015, a destructive MW 7.8 earthquake struck the capital of Nepal,
Kathmandu, killing more than 8800 people and destroying numerous historical structures …