Results 91 to 100 of about 2,343 (216)
Seismogenic structures and active creep in the Granada Basin (S-Spain)
program (PPJIA2023-002)
Stich, Daniel +7 more
openaire +2 more sources
野外地质调查发现金沙江断裂带北段麦宿断裂附近发育长约50 km的地震地表破裂带,其最大垂直位移为2 m。基于该地震地表破裂带周围架设的密集地震台阵于2020 年 12 月至 2022 年 7 月期间记录到的连续波形数据,采用双差定位方法对(31.55°N—31.85°N,98.31°E—98.98°E) 区域内的578个地震事件进行定位,并利用基于P波初动的HASH方法对定位得到的地震事件进行震源机制解反演,获得了37组震源机制解 ...
Yifeng Wu, Fangtou Tang, Xudong Jiang
doaj +1 more source
Seismogenic frictional melting in the magmatic column
Lava dome eruptions subjected to high extrusion rates commonly evolve from endogenous to exogenous growth and limits to their structural stability hold catastrophic potential as explosive eruption triggers.
K.-U. Hess +8 more
core +1 more source
The Mw 7.0 Dingri earthquake, which occurred on 7 January 2025, occurred at the southern end of the Xainza-Dinggyê Fault Zone within the South Tibet Rift (STR) system, in the Dengmecuo graben.
Qingyi Liu +6 more
doaj +1 more source
Hazard in the Gulf of Cadiz: review of the large seismogenic structures
The Gulf of Cadiz is located at the SW Iberian Margin and hosts the African-Eurasian plate boundary. This is one of the most seismogenic areas in Western Europe, where historical and instrumental earthquakes occurred, ranging from Mw 6 to 8.5, and some of them triggered destructive tsunamis.
Sànchez-Serra, Cristina +7 more
openaire +1 more source
By systemic processing, comprehensive analysis, and interpretation of gravity data, we confirmed the existence of the west segment of the coastal fault zone (west of Yangjiang to Beibu Bay) in the coastal region of South China.
Lisi Bi +4 more
doaj +1 more source
联合InSAR和热红外技术研究2023年甘肃积石山MS6.2地震构造活动特征
联合使用合成孔径雷达干涉测量(InSAR)与热红外遥感技术,系统分析了2023年甘肃积石山MS6.2地震的同震形变场、发震断层参数、滑动分布、库仑应力变化及震前热异常特征。利用Sentinel-1A升降轨合成孔径雷达数据,通过差分干涉测量获取了积石山地震的同震形变场,结果表明:形变以抬升为主,升、降轨最大雷达视线向位移分别约为6.5 cm和7.2 cm,形变区集中分布于拉脊山南、北缘断裂之间。采用四叉树采样与贝叶斯反演方法,在合理模型约束下,反演得到积石山地震发震断层的几何参数为:走向324°±1 ...
Bingdun Yan +9 more
doaj +1 more source
The Hikurangi subduction margin, New Zealand, has not experienced any significant (>Mw 7.2) subduction interface earthquakes since historical records began ∼170 years ago.
Martin Reyners +64 more
core +1 more source
On 7 January 2025, at Beijing time, an Mw7.1 earthquake occurred in Dingri County, Shigatse, Tibet. To accurately determine the fault that caused this earthquake and understand the source mechanism, this study utilized Differential Interferometric ...
Shuyuan Yu +4 more
doaj +1 more source
Tectonic history of seismogenic fault structures in Central Iran [PDF]
S. Beygi, A. Nadimi, H. Safaei
openaire +1 more source

