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Monitoring of Local Earthquakes in Haiti Using Low‐Cost, Citizen‐Hosted Seismometers and Regional Broadband Stations
Short‐Range Recordings of Shallow Underwater Explosions with Short‐Period and Broadband Seismometers in the Bay of Hyères, France
Rupture Segmentation of the 14 August 2021 M w 7.2 Nippes, Haiti, Earthquake Using Aftershock Relocation from a Local Seismic Deployment
The Western Gulf of Corinth (Greece) 2020–2021 Seismic Crisis and Cascading Events: First Results from the Corinth Rift Laboratory Network
Preparing for InSight: Evaluation of the Blind Test for Martian Seismicity
Numerical and Empirical Simulation of Linear Elastic Seismic Response of a Building: The Case of Nice Prefecture
Site Effects in Port‐au‐Prince (Haiti) from the Analysis of Spectral Ratio and Numerical Simulations
P ‐Delays from Floating Seismometers (MERMAID), Part I: Data Processing
SI-Hex: a new catalogue of instrumental seismicity for metropolitan France
High‐Frequency Directivity Effect for an M w 4.1 Earthquake, Widely Felt by the Population in Southeastern France
Crustal Structure and Fault Geometry of the 2010 Haiti Earthquake from Temporary Seismometer Deployments
The GROSMarin experiment: three dimensional crustal structure of the North Ligurian margin from refraction tomography and preliminary analysis of microseismic measurements
Joint multidisciplinary study of the Saint-Sauveur–Donareo fault (lower Var valley, French Riviera): a contribution to seismic hazard assessment in the urban area of Nice
Moment-Tensor Determination by Nonlinear Inversion of Amplitudes
Focal Mechanisms from Sparse Observations by Nonlinear Inversion of Amplitudes: Method and Tests on Synthetic and Real Data
Interpretation of Broadband Ocean-Bottom Seismometer Horizontal Data Seismic Background Noise
A Two-Stage Method for Ground-Motion Simulation Using Stochastic Summation of Small Earthquakes
Geodynamic setting of Izu–Bonin–Mariana boninites
Abstract The Izu-Bonin-Mariana (IBM) forearc is characterized by the occurrence of boninite-like lavas. The study of the Cenozoic setting of the genesis of these boninitic lavas in light of modern geodynamic contexts in the Tonga and Fiji regions lead us to define three tectonic settings that favour the formation of boninites in back-arc basins in addition to previous settings that involve the presence of a mantle plume: (1) propagation at low angle between a spreading centre and the associated volcanic arc; (2) intersection at a high angle of an active spreading centre and a transform fault at the termination of an active volcanic arc; and (3) intersection at a right angle between an active spreading centre and a newly created subduction zone. A geodynamic model of the Philippine Sea Plate shows that boninites in the Bonin Islands are related to the second mechanism mentioned above, whereas Mariana forearc boninites are relevant to the third mechanism. In the early Eocene, the transform plate boundary bounding the eastern margin of the Philippine Sea Plate at the location of the present-day Mariana arc evolved into a subduction zone that trends perpendicular to the active spreading centre of the West Philippine Basin, somewhere around 43–47 Ma. The presence of a mantle plume in the vicinity of the subduction zone bounding the northern IBM arc explains boninites that erupted in its northern part, but only in early Eocene time.