Results 41 to 50 of about 2,046 (134)
State of Stress Across Major Faults in the Nankai Subduction Zone Estimated From Wellbore Breakouts
Abstract Quantifying the orientation and magnitude of stress at tectonically active margins and along major fault systems is integral to understanding the mechanics of faulting and earthquakes. Here we use data collected as part of the IODP (Integrated Ocean Drilling Program) Nankai Trough Seismogenic Zone Experiment to constrain in situ stress ...
Kaitlin E. Schaible, Demian M. Saffer
wiley +1 more source
Sea Water Aging ofGlass Reinforced Composites:Shear Behaviour andDamage Modelling [PDF]
International audienceThis paper presents results from a study of the wet aging of four thermoset resins and their [0°/90°] stitched glass fibre reinforced composites.
Casari, P., Davies, Peter, Mazéas, F.
core +4 more sources
Abstract Magmatism is a known driver of flank instability at volcanoes where flank slip has been observed. Studies of instability at Kı̄lauea, Piton de la Fournaise, and Etna imply that long‐term flank motion likely requires the presence of a layer accommodating the sliding, and a force, such as magma intrusion, that promotes slip.
J. Gonzalez‐Santana +3 more
wiley +1 more source
Energy partitioning during an earthquake [PDF]
We investigate the partitioning of energy released during an earthquake to radiated, fracture and thermal energies in an attempt to link various observational results obtained in different disciplines.
Kanamori, Hiroo, Rivera, Luis
core +1 more source
Abstract Polygonal Fault Systems (PFS) or networks were generated in 3D finite‐difference models within the upper (active) layer of two‐layer model. The driving force of this process results from a progressive diagenetically induced volumetric contraction (porosity reduction) of the active layer during its burial.
A. I. Chemenda, G. Ballas, A. Gay
wiley +1 more source
Abstract The Ramapo Seismic Zone (RSZ) in the Northeastern United States hosts frequent but poorly understood intraplate earthquakes, potentially posing a significant hazard to the nearby New York metropolitan area. The 5 April 2024, Mw ${M}_{w}$4.8, Tewksbury, New Jersey earthquake, provides a rare opportunity to study the RSZ seismicity.
Eric Beaucé +4 more
wiley +1 more source
A new approach to profiling taphonomic history through bone fracture analysis, with an example application to the Linearbandkeramik site of Ludwinowo 7. [PDF]
This is the author accepted manuscript. The final version is available from the publisher via the DOI in this record.This paper presents a new method of assessing and displaying taphonomic history through detailed bone fracture analysis.
Johnson, EV, Outram, AK, Parmenter, PCR
core +1 more source
This paper studies the distribution characteristics of the current in situ stress field in northeast Yunnan Province by using multisource stress data, including in situ stress measurements, focal mechanism solutions, and borehole damage information, and comprehensively determines the in situ stress magnitude and direction in the mining area.
Hui Wang +6 more
wiley +1 more source
Abstract Seismic faults are surrounded by damaged rocks with reduced rigidity and enhanced attenuation. These damaged fault zone structures can amplify seismic waves and affect earthquake dynamics, yet they are typically omitted in physics‐based regional ground motion simulations.
Nico Schliwa +2 more
wiley +1 more source
A Stress Memory Effect in Olivine at Upper Mantle Pressures and Temperatures
Abstract Cyclic deformation experiments on olivine aggregates have been conducted at pressures of 1.9–2.8 GPa and temperatures of 297–1250 K. Measurements of mechanical data combined with acoustic emission (AE) monitoring revealed that activity of AE increased with differential stress and ceased once loading was halted in the anelastic regime.
T. Ohuchi +15 more
wiley +1 more source

