Results 51 to 60 of about 1,280 (178)
The Zhangjiakou-Bohai Seismic Belt (ZBSB) is a crucial intraplate seismic belt in Eastern China, covering densely populated and economically developed regions with significant seismic hazards.
Yuyang Zhang +6 more
doaj +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
Genesis of continental seismogenic zone and a new fault zone model
Experiments were conducted repeatedly on Mannari granite under different temperature and confining pressure conditions. Systematic micro- and submicro-structural and mechanical analyses of granite samples deformed under 1.5 GPa (confining pressure), at 25°C–650°C temperatures and at 2×10−6s−1 strain rate show the brittle-ductile deformation ...
Junlai Liu, M. Shimada
openaire +1 more source
Back‐Propagating Earthquake Rupture Controlled by Fluid‐Modulated Effective Normal Stress
Abstract Back‐propagating earthquake rupture (BPR), where slip migrates opposite to the main rupture direction, is observed in several earthquakes but its origin remains poorly understood, particularly the role of fluids. We use dynamic simulations of frictional sliding coupled with fluids to explore the mechanisms of BPR. Our simulations show that BPR
Jiayi Ye +2 more
wiley +1 more source
Fault Geometrical Control on Fault Slip: Experimental Validation of Theoretical Models
Abstract Slip distribution along tectonic faults is recognized as highly heterogeneous across all spatial scales and is linked to various aspects of the earthquake cycle, such as aftershock density and stress‐drop variability. A key factor often considered to control slip heterogeneity is the fault geometry, which is typically nonplanar at various ...
Tom Gabrieli +3 more
wiley +1 more source
The silent earthquake of 2002 in the Guerrero seismic gap, Mexico (Mw=7.6): Inversion of slip on the plate interface and some implications [PDF]
We invert GPS position data to map the slip on the plate interface during an aseismic, slow-slip event, which occurred in 2002 in the Guerrero seismic gap of the Mexican subduction zone, lasted for ~4 months, and was detected by 7 continuous GPS ...
S. I. Franco-Sánchez +6 more
doaj
Tectonic Tremor Reveals Slow Deformation Along the Antarctic–South American Subduction Zone
Abstract The Antarctic–South American subduction zone is among the least explored convergent margins and lacks documented large interplate earthquakes despite ongoing convergence. Here we report the discovery of tectonic tremor along this plate boundary using continuous seismic data.
K. Azúa, S. Ruiz, S. Ide
wiley +1 more source
InSAR coseismic deformation and seismogenic structure of the 2023 MW6.9 Tajikistan earthquake
An earthquake of magnitude 6.9 occurred in Tajikistan on February 23, 2023. Studying this earthquake is the key to understanding the seismogenic structure of this area. The slip distribution of the MW6.9 earthquake was inverted using InSAR technology and
Rongliu Chen +5 more
doaj +1 more source
Structural control and system-level behavior of the seismic cycle at the Nankai Trough
The Nankai Trough in Southwest Japan exhibits a wide spectrum of fault slip, with long-term and short-term slow-slip events, slow and fast earthquakes, all associated with different segments down the plate interface.
Qibin Shi +5 more
doaj +1 more source
Abstract The 2025 Mw7.1 Dingri earthquake is the largest normal‐faulting event in southern Tibetan plateau recorded with near‐field observations. By integrating back‐projection imaging, multi‐point‐source inversion, and finite‐fault modeling, we reveal that the rupture propagated at variable speeds in a cascading manner across a complex conjugate fault
Qi Li +8 more
wiley +1 more source

