Results 41 to 50 of about 216 (161)
Iwo‐yama volcano, part of the Kirishima Volcanic Complex, has recently shown signs of unrest. We conducted a hypocenter relocation of shallow earthquakes and broadband magnetotelluric measurements around Iwo‐yama.
K. Tsukamoto +8 more
doaj +1 more source
Validation of ShakeMaps Created From Global Navigation Satellite System (GNSS) Velocities
Ground velocity observations generated through a time difference of Global Navigation Satellite Systems (GNSS) phase observables and orbits have been shown to be comparable to seismic recordings without clipping during intense ground motions. Computing GNSS velocities is also computationally scalable and increases the density of ground motion ...
Jensen V. DeGrande, Brendan W. Crowell
wiley +1 more source
Western Kanagawa, located in eastern Japan, has repeatedly experienced M-8 class megathrust earthquakes, referred to as Kanto earthquakes, within a tectonic setting characterized by the NNW-ward subduction of Philippine Sea plate. On 9 August 2024, an Mw
Yasunori Sawaki +2 more
doaj +1 more source
Abstract Caldera systems commonly experience inner resurgence, which shapes patterns of volcanic activity. However, incomplete reconstructions of past ground deformation can lead to incorrect recognition of precursory signals. The Campi Flegrei caldera (Italy) provides an exceptional opportunity to address this issue as uplifted marine sediments ...
Jacopo Natale, Stefano Vitale
wiley +1 more source
Hypocenter Relocation in the Cianjur Region Using the Double-Difference Method
Abstract Indonesia’s seismicity results from the collision of the Eurasian, Indo-Australian, and Pacific plates, and the Cianjur region in West Java lies at the nexus of active faults and the southern Java subduction zone. To refine hypocenter locations and bolster seismic-hazard assessments, we applied the Double-Difference ...
Eko Minarto +2 more
openaire +1 more source
Step-wise relocation of ISC earthquake hypocenters for linearized tomographic imaging of slab structure [PDF]
A vast volume of seismic phase data, computed from routinely determined hypocenter locations, is presently available for seismic imaging techniques such as tomographic inversion and residual sphere analysis. Routinely reported earthquake hypocenters, however, can be in error by several tens of kilometers.
Hilst, R.D. van der, Engdahl, E.R.
openaire +2 more sources
The Maros-Pangkep region in South Sulawesi is a tropical karst landscape not officially mapped as an active fault zone, yet it has exhibited increasing micro-seismic activity in recent years.
Kevin Hanyu Clinton Wulur +4 more
doaj +1 more source
Abstract Normal faults in southern Tibet have long suffered from limited ground‐based seismic and geodetic observations, constraining our understanding of both interseismic and coseismic processes and their interactions. The 2025 Mw 7.1 Dingri earthquake provides an opportunity to address these gaps.
Haicheng Xiong +9 more
wiley +1 more source
Source models for the 2016 Mw6.0 Hutubi earthquake, Xinjiang, China: A possible reverse event
South and north-dipping nodal planes from the U.S. Geological Survey moment tensor solution were used to invert global teleseismic body waves to reveal the source rupture process of the December 8, 2016, Mw6.0 Hutubi earthquake.
Gang Liu +5 more
doaj +1 more source
Abstract Fault slip occurs in both seismic and aseismic styles with spatial variability across scales, yet non‐unique source inference limits our ability to resolve slip complexity and dynamics. Here we evaluate the effect of spatial smoothing regularization in Bayesian frameworks by comparing an unregularized (BUR) approach that samples distributed ...
Xiong Zhao, Junle Jiang
wiley +1 more source

