Results 211 to 220 of about 63,820 (273)
Abstract We analyze Interferometric Synthetic Aperture Radar (InSAR) and Global Navigation Satellite System (GNSS) data to characterize ground deformation and dike opening associated with the May 2021 Nyiragongo eruption. Despite documented eruptions in 1977 and 2002, Nyiragongo's magmatic system and its interaction with regional rifting remain poorly ...
D. Murekezi +9 more
wiley +1 more source
Abstract Ocean bottom pressure recordings are a key observation for both ocean circulation and seafloor geodesy. New self‐calibrating instruments may solve a long‐time issue of instrument drift, allowing new high precision observations. However, instruments on the seafloor may settle over days to months, potentially contaminating results.
Nicholas Harmon +8 more
wiley +1 more source
Abstract This study reveals different slip patterns of tsunami sources between two prehistoric giant earthquakes along the southern Kuril Trench, based on an integration of geological data and numerical simulations. The most recent giant earthquake occurred in the 17th century and its predecessor was in the 13th–14th century.
Kei Ioki +7 more
wiley +1 more source
Channelization Versus Retardation During Trace Element Segregation in Compaction‐Driven Fluid Flow
Abstract The migration of fluids, such as aqueous fluids and melts, is often channelized and crucial for trace element transport. However, trace elements typically migrate slower than the fluid due to partitioning between solid and fluid phases, known as retardation.
Stefan M. Schmalholz +4 more
wiley +1 more source
Systematic deficiency of aftershocks in areas of high coseismic slip for large subduction zone earthquakes. [PDF]
Wetzler N +3 more
europepmc +1 more source
Modelling subduction zone magmatism
Subduction zone magmatism is a well studied area due to dangerous consequences of volcanic\ud activity at subduction zones. Whilst it is widely accepted that water leaving the slab causes\ud the magmatism, the method in which the water leaves the slab and causes magmatism is\ud unclear.
openaire
Abstract The structure and properties of mature upper oceanic plates may evolve through mechanisms such as magmatism, hydrothermal circulation, and faulting. However, high‐resolution constraints, especially those involving both P‐ and S‐waves, remain scarce, limiting our ability to detect these processes and assess their impacts on crustal properties ...
Anne Bécel +3 more
wiley +1 more source
Delineating the Central Anatolia Transition Zone (CATZ): Constraints from Integrated Geodetic (GNSS/InSAR) and Seismic Data. [PDF]
Kutoğlu ŞH, Akgün E, Softa M.
europepmc +1 more source
Bridging the gap between subduction dynamics and the long-term strength of the Sunda megathrust. [PDF]
Capitanio FA +6 more
europepmc +1 more source
Rift linkage and inheritance determine collisional mountain belt evolution. [PDF]
Wolf SG, Huismans RS, Muñoz JA, May DA.
europepmc +1 more source

