Overview of topographic effects based on experimental observations: meaning, causes and possible interpretations

M Massa, S Barani, S Lovati - Geophysical Journal International, 2014 - academic.oup.com
The paper presents an extensive review of topographic effects in seismology taking into
account the knowledge of 40 yr of scientific literature. An overview of topographic effects …

Three-dimensional full waveform inversion of short-period teleseismic wavefields based upon the SEM–DSM hybrid method

V Monteiller, S Chevrot, D Komatitsch… - Geophysical Journal …, 2015 - academic.oup.com
We present a method for high-resolution imaging of lithospheric structures based on full
waveform inversion of teleseismic waveforms. We model the propagation of seismic waves …

Scattering of high-frequency seismic waves caused by irregular surface topography and small-scale velocity inhomogeneity

S Takemura, T Furumura… - Geophysical Journal …, 2015 - academic.oup.com
Based on 3-D finite difference method simulations of seismic wave propagation, we
examined the processes by which the complex, scattered high-frequency (f> 1 Hz) seismic …

Seismic modelling and observations of rainfall

M Bakker, C Legout, F Gimbert, G Nord… - Journal of …, 2022 - Elsevier
Rainfall is a key driver of geomorphological processes ranging from impacting drops that
lead to the small-scale dislodgement of soil particles to large-scale morphogenic floods and …

Magmatic and sedimentary structure beneath the Klyuchevskoy volcanic group, Kamchatka, from ambient noise tomography

RG Green, C Sens‐Schönfelder… - Journal of …, 2020 - Wiley Online Library
Abstract The Klyuchevskoy Volcanic Group is a cluster of the world's most active subduction
volcanoes, situated on the Kamchatka Peninsula, Russia. The volcanoes lie in an unusual …

Topography effect on ambient noise tomography: a case study for the Longmen Shan area, eastern Tibetan Plateau

R Jin, X He, H Fang, J Xie, Y Liu… - Geophysical Journal …, 2023 - academic.oup.com
Ambient noise tomography (ANT) is a widely used method to obtain shear wave velocity
structure in the crust and upper mantle. Usually, the topography is assumed to have …

Back‐arc extension of the Central Bransfield Basin induced by ridge–trench collision: Implications from ambient noise tomography and stress field inversion

W Li, X Yuan, B Heit… - Geophysical …, 2021 - Wiley Online Library
Abstract The Bransfield Basin is a young (∼ 4 Ma) back‐arc basin related to the remnant
subduction of the Phoenix Plate that once existed along the entire Pacific margin of the …

Crustal characterization of the Hengill geothermal fields: Insights from isotropic and anisotropic seismic noise imaging using a 500‐node array

SM Wu, P Sánchez‐Pastor… - Journal of …, 2024 - Wiley Online Library
The Hengill volcano and its associated geothermal fields represent Iceland's most
productive harnessed high‐temperature geothermal fields, where resources are fueled by …

3D wave-equation dispersion inversion of Rayleigh waves

Z Liu, J Li, SM Hanafy, G Schuster - Geophysics, 2019 - library.seg.org
The 2D wave-equation dispersion (WD) inversion method is extended to 3D wave-equation
dispersion inversion of surface waves for the shear-velocity distribution. The objective …

The deep structure of the Scandes and its relation to tectonic history and present-day topography

V Maupin, A Agostini, I Artemieva, N Balling… - Tectonophysics, 2013 - Elsevier
We review the results of the TopoScandiaDeep project, a component of the TOPOEUROPE
project, in which we have studied the crustal and upper mantle structures of southern …