Turnitin
降AI改写
早检测系统
早降重系统
Turnitin-UK版
万方检测-期刊版
维普编辑部版
Grammarly检测
Paperpass检测
checkpass检测
PaperYY检测
Seismic wavefield imaging of Earth's interior across scales
Seismic full-waveform inversion (FWI) for imaging Earth's interior was introduced in the late
1970s. Its ultimate goal is to use all of the information in a seismogram to understand the …
1970s. Its ultimate goal is to use all of the information in a seismogram to understand the …
Slow slip events in New Zealand
Continuously operating global positioning system sites in the North Island of New Zealand
have revealed a diverse range of slow motion earthquakes on the Hikurangi subduction …
have revealed a diverse range of slow motion earthquakes on the Hikurangi subduction …
Body wave extraction and tomography at Long Beach, California, with ambient‐noise interferometry
We retrieve P diving waves by applying seismic interferometry to ambient‐noise records
observed at Long Beach, California, and invert travel times of these waves to estimate 3‐DP …
observed at Long Beach, California, and invert travel times of these waves to estimate 3‐DP …
Large-scale dynamic triggering of shallow slow slip enhanced by overlying sedimentary wedge
Slow slip events have become recognized in the last decade as an important mode of fault
slip, and are most widely observed at subduction zones. Many episodes of tectonic tremor …
slip, and are most widely observed at subduction zones. Many episodes of tectonic tremor …
Joint data and model-driven simultaneous inversion of velocity and density
Density is an important parameter for both geological research and geophysical exploration.
However, for model-driven seismic inversion methods, high-fidelity density inversion is …
However, for model-driven seismic inversion methods, high-fidelity density inversion is …
A review of shallow slow earthquakes along the Nankai Trough
Slow earthquakes occur at deep and shallow plate boundaries along the Nankai Trough.
Deep slow earthquakes are continuously distributed along the 30–40 km depth contours of …
Deep slow earthquakes are continuously distributed along the 30–40 km depth contours of …
Elevated pore pressure and anomalously low stress in regions of low frequency earthquakes along the Nankai Trough subduction megathrust
Recent seismic reflection and ocean bottom seismometer (OBS) studies reveal broad
regions of low seismic velocity along the Nankai subduction plate boundary megathrust …
regions of low seismic velocity along the Nankai subduction plate boundary megathrust …
Inversion strategies for visco-acoustic waveform inversion
Visco-acoustic waveform inversion can potentially yield quantitative images of the
distribution of both velocity and the attenuation parameters from seismic data. Intrinsic P …
distribution of both velocity and the attenuation parameters from seismic data. Intrinsic P …
Tsunami excitation in the outer wedge of global subduction zones
The world's most devastating local and ocean-wide tsunamis are generated by subduction
zone earthquakes, but the mechanisms for powerful seafloor uplift and tsunami generation …
zone earthquakes, but the mechanisms for powerful seafloor uplift and tsunami generation …
[HTML][HTML] Pore pressure distribution of a mega-splay fault system in the Nankai Trough subduction zone: Insight into up-dip extent of the seismogenic zone
We use the pore pressure distribution predicted from a waveform tomography (WT) velocity
model to interpret the evolution of the mega-splay fault system in the Nankai Trough off …
model to interpret the evolution of the mega-splay fault system in the Nankai Trough off …