Results 231 to 240 of about 145,917 (290)
A yield design approach to the stability analysis of A seabed subjected to wave loading and pseudo-static seismic forces. [PDF]
Quiuqui JPC, Maghous S.
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Shaking table test of isolated and non-isolated low-rise masonry structure. [PDF]
Yao Z, Ruoxi W, Youchao Z.
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Studies of Geosphere Interactions by Means of Laser Interference Complex. [PDF]
Dolgikh G, Budrin S, Dolgikh S.
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Gemini: the first underground testbed for seismic isolation and inter-platform control in next-generation gravitational-wave detectors. [PDF]
Andric T +20 more
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Seismic waves and seismic barriers
Acoustical Physics, 2011The basic idea of seismic barrier is to protect an area occupied by a building or a group of buildings from seismic waves. Depending on nature of seismic waves that are most probable in a specific region, different kinds of seismic barriers are suggested.
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Multiple scattering of seismic waves
Ultrasonics, 2002We present theory and numerical simulations to model seismic wave propagation in the Earth crust. We compare them to observations made in Mexico.
N, Trégourès +6 more
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Seismic wave modeling for seismic imaging
The Leading Edge, 2009Many scientific applications require accurate modeling of seismic wave propagation in complex media. These objectives can include fundamental understanding of seismic wave propagation of the Earth on a global scale, including fluid envelopes, mitigation of seismic risk with better quantitative estimates of seismic hazard, and improved exploitation of ...
Virieux, J. +7 more
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1956
When an earthquake occurs, energy, which may reach the order of 1025 ergs in the greatest earthquakes is released, within a few seconds or less, from a focal region inside the Earth whose linear dimensions may be of the order of several kilometres. The (somewhat indefinite) centre of the focal region is called the focus.
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When an earthquake occurs, energy, which may reach the order of 1025 ergs in the greatest earthquakes is released, within a few seconds or less, from a focal region inside the Earth whose linear dimensions may be of the order of several kilometres. The (somewhat indefinite) centre of the focal region is called the focus.
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SEG Technical Program Expanded Abstracts 1987, 1987
This paper presents a multichannel method for enhancing the signal-to-noise ratio, when the noise is purely random. We show that under some assumptions the contribution of each wave may be individualized. The quality of the results is sensitive to the estimation of the interspectral matrix from the initial traces.
Jerome Mars +4 more
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This paper presents a multichannel method for enhancing the signal-to-noise ratio, when the noise is purely random. We show that under some assumptions the contribution of each wave may be individualized. The quality of the results is sensitive to the estimation of the interspectral matrix from the initial traces.
Jerome Mars +4 more
openaire +1 more source

