Results 71 to 80 of about 1,799 (182)

Wave field inversion of ambient seismic noise

open access: yesProceedings, 2017
We formulate a full wave field inversion for ambient seismic noise recorded by large and dense seismograph arrays. Full wave field inversion exploits the constraints on the gradients of the wave field that array data inherently possess (the sum is greater than its parts). Consequently, we can relax the spatial and temporal constraints on the wave field
De Ridder, S, Maddison, JR
openaire   +2 more sources

Assessing the Main Frequencies of Modern and Historical Buildings Using Ambient Noise Recordings: Case Studies in the Historical Cities of Crete (Greece)

open access: yesHeritage, 2018
Monitoring seismic structural response is an essential issue in earthquake risk assessments and mitigation studies for monumental buildings in order to undertake earthquake disaster management.
Margarita Moisidi   +2 more
doaj   +1 more source

Reflection images from ambient seismic noise

open access: yesGeophysics, 2009
Abstract One application of seismic interferometry is to retrieve the impulse response (Green's function) from crosscorrelation of ambient seismic noise. Various researchers show results for retrieving the surface-wave part of the Green's function. However, reflection retrieval has proven more challenging.
Draganov, D.S. (author)   +4 more
openaire   +4 more sources

Spatio-temporal changes in the seismic velocity induced by the 2011 Tohoku-Oki earthquake and slow slip event revealed from seismic interferometry, using ocean bottom seismometer’s records

open access: yesProgress in Earth and Planetary Science, 2018
Seismic interferometry is one of the most effective techniques for detecting temporal variations in seismic velocity caused by large earthquakes. Before the 2011 Tohoku-Oki earthquake (M w 9.0) near the Japan Trench, a slow slip event (SSE, M w 7.0) and ...
Miyuu Uemura   +4 more
doaj   +1 more source

Ambient seismic noise tomography of the Antarctic continent [PDF]

open access: yes, 2019
The lithosphere of Antarctica reacts to both the stress variations due to the dynamics of the mantle and the variation of the glacial load due to changes in climate. These two factors act on the dynamics of the glacial mass, on the evolution of the continent's topography and on the plate seismicity.
openaire   +1 more source

Monitoring diffuse volcanic degassing with seismic ambient noise [PDF]

open access: yesNatural Hazards and Earth System Sciences
Diffuse volcanic degassing is a persistent and often underestimated natural hazard, with potential impacts on air quality, ecosystem health, and volcanic risk management.
H. Seivane, H. Seivane, M. Schimmel
doaj   +1 more source

Seismic Ambient Noise [PDF]

open access: yesThe Journal of the Acoustical Society of America, 2019
openaire   +2 more sources

Seismic response of a slow-moving landslide: exploring data from two years of seismic monitoring at the Hollin Hill Landslide Observatory (UK)

open access: yesSeismica
Early-warning of landslide failure relies on understanding subsurface processes that drive slope destabilisation, including changes in moisture content or mechanical behaviour.
Arnaud Watlet   +8 more
doaj   +1 more source

Moho Imaging with Fiber Borehole Strainmeters Based on Ambient Noise Autocorrelation

open access: yesSensors
Moho tomography is important for studying the deep Earth structure and geodynamics, and fiber borehole strainmeters are broadband, low-noise, and attractive tools for seismic observation. Recently, many studies have shown that fiber optic seismic sensors
Guoheng Qi   +4 more
doaj   +1 more source

Home - About - Disclaimer - Privacy