Seismic and electrical signatures of the lithosphere–asthenosphere system of the normal oceanic mantle
Although plate tectonics started as a theory of the ocean basins nearly 50 years ago, the
mechanical details of how it works are still poorly known. Our understanding of these details …
mechanical details of how it works are still poorly known. Our understanding of these details …
Overpressured underthrust sediment in the Nankai Trough forearc inferred from transdimensional inversion of high‐frequency teleseismic waveforms
Active‐source seismic surveys have resolved the fine‐scale P‐wave velocity (Vp) of the
subsurface structure in subduction forearcs. In contrast, the S‐wave velocity (Vs) structure is …
subsurface structure in subduction forearcs. In contrast, the S‐wave velocity (Vs) structure is …
Lithospheric imaging through reverberant layers: Sediments, oceans, and glaciers
The Earth, in large portions, is covered in oceans, sediments, and glaciers. High‐resolution
body wave imaging in such environments often suffers from severe reverberations, that is …
body wave imaging in such environments often suffers from severe reverberations, that is …
Crustal structure beneath the Alcock Seamount in the Andaman Sea
Alcock and Sewell seamounts are important geomorphic features in the Andaman Sea due
to their association with the tectonic history of the Sunda subduction zone. Despite the …
to their association with the tectonic history of the Sunda subduction zone. Despite the …
The signature and elimination of sediment reverberations on submarine receiver functions
While the receiver function technique has been successfully applied to high‐resolution
imaging of sharp discontinuities within and across the lithosphere, it suffers from severe …
imaging of sharp discontinuities within and across the lithosphere, it suffers from severe …
Characterization of crustal and uppermost‐mantle seismic discontinuities in the Ontong Java Plateau
Abstract The Early Cretaceous Ontong Java Plateau (OJP) in the southwestern Pacific
Ocean is the largest oceanic plateau by volume on Earth, and a broad range of observations …
Ocean is the largest oceanic plateau by volume on Earth, and a broad range of observations …
Crustal Imaging with Noisy Teleseismic Receiver Functions Using Sparse Radon Transforms
The receiver function (RF) is a widely used crustal imaging technique. In principle, it
assumes relatively noise‐free traces that can be used to target receiver‐side structures …
assumes relatively noise‐free traces that can be used to target receiver‐side structures …
A fluid‐rich layer along the Nankai trough megathrust fault off the Kii Peninsula inferred from receiver function inversion
Investigation of fluid distribution along megathrust faults is an important issue, since the fluid
affects frictional properties and thus slip behavior on faults. Scattered teleseismic phases, or …
affects frictional properties and thus slip behavior on faults. Scattered teleseismic phases, or …
Prediction of shear-wave velocity using receiver functions based on the deep learning method
TW YANG, DP CAO, NQ DU, RA CUI, FZ NAN… - Chinese Journal of …, 2022 - en.dzkx.org
The teleseismic receiver function contains a lot of information on converted PS waves and
multiple reflections generated by velocity discontinuities below stations, which is widely …
multiple reflections generated by velocity discontinuities below stations, which is widely …
[HTML][HTML] Numerical Modeling on Ocean-Bottom Seismograph P-Wave Receiver Function to Analyze Influences of Seawater and Sedimentary Layers
W Gong, H Hu, A Ruan, X Niu, W Wang… - Journal of Marine Science …, 2024 - mdpi.com
It is challenging to apply the receiver function method to teleseisms recorded by ocean-
bottom seismographs (OBSs) due to a specific working environment that differs from land …
bottom seismographs (OBSs) due to a specific working environment that differs from land …