Results 171 to 180 of about 96,657 (309)
Seismological Models, mineral physics and spin transitions in the lower mantle
B. L. N. Kennett
openalex +1 more source
Spectral analysis for the inference of noisy Hawkes processes
Abstract Classic estimation methods for Hawkes processes rely on the assumption that observed event times are indeed a realization of a Hawkes process, without considering any perturbation of the model. In practice, observations are often altered by some noise, and so we consider, in this work, the observations to be the indistinguishable union of ...
Anna Bonnet +3 more
wiley +1 more source
Dike Arrest Identification by Reverse Focal Mechanisms: Evidence From Etna Eruptions
Abstract Real‐time prediction of dike behavior during an eruption remains a significant challenge. Determining the timing and location of dike propagation arrest is crucial for hazard evaluation. The inherent complexity of eruptive phenomena makes rapid, unambiguous interpretation through modeling difficult.
Alessandro Bonaccorso +2 more
wiley +1 more source
Abstract The Pamir Plateau stands out at the westernmost Tibetan Plateau as a north‐facing convex promontory, bordering the tectonically rejuvenated Tianshan orogen. To understand the mode of crustal deformation, we analyze crustal anisotropy in the Pamir‐Tianshan using shear wave splitting of the Moho‐converted phases.
Wei Li +4 more
wiley +1 more source
Abstract The Gulf of Aqaba (GoA) is the seismically most active region in the Red Sea, with a history of large earthquakes and posing a high seismic hazard to coastal communities. This study uses back‐projection and dynamic rupture simulation to investigate the largest instrumentally recorded earthquake in the GoA, the 1995 Mw ${M}_{\mathrm{w}}$ 7.2 ...
Bo Li +6 more
wiley +1 more source
Seismology of an Ensemble of ZZ Ceti Stars [PDF]
J. C. Clemens +3 more
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Dip Angles of Mountain‐Front Facets Encode Long‐Term Slip Rates Along the Wasatch Normal Fault, USA
Abstract Mountains bounded by seismogenic normal faults are commonly decorated with facet slopes: planar slopes made of bedrock, or bedrock mantled by regolith, that rise above the fault. The steepness of such slopes is thought to reflect a balance between fault slip and erosion rate.
William T. Struble +5 more
wiley +1 more source
Seismogenic strength and anatomy of mahendragarh-dehradun fault: implication to seismic risk. [PDF]
Gera SK +4 more
europepmc +1 more source

