seismic waves

(also known as a quake, tremor, or temblor) is the result of a sudden release of energy in the Earth's crust that creates seismic waves.

Seismic waves are waves that travel through the Earth, most often as the result of a tectonic earthquake, sometimes from an explosion.

An earthquake is the result of a sudden release of energy in the Earth's crust that creates seismic waves.

Results indicated most of the permanent ground displacements occurred within a few minutes of the arrival of the first seismic waves.

Caitlin believes the seismic waves are felt in the toenails and move up to the ear via bone conduction.

The slope has amplification effect to input seismic waves, and the effect become extremely prominent around the crest of the slope.

When an earthquake occurs, it releases energy in the form of seismic waves that radiate from the earthquake source in all directions.

The Tunguska event included seismic waves and infrasonic disturbances that were recorded around the world.

The tremendous heat causes rapid expansion of a spherical cavity, which in turn generates seismic waves.

One segment of this field is devoted to seismology, the study of seismic waves that are generated when major geological shifts occur.

The converter station valve hall with suspension-mass is nonlinear analyzed as the structure is afforded different seismic waves.

The seismic waves signal detected by sensors is principally Rayleigh wave when the detection position is far from the target.

In zones where earthquakes are known to occur, improved construction techniques can significantly reduce the effects of seismic waves.

Third, all died of AIDS are very weak physical, which can be weak physical death, when the seismic waves.

Attenuation of seismic waves between such surfaces can be similarly diagnostic.

The oil and gas driller can send seismic waves miles under the sea floor, gather the echoes, and deduce whether petroleum might exist there.

But on soft soils, vibrations from long-period seismic waves are amplified, possibly exacerbating the swaying of skyscrapers.

The mitigation effect of maximal velocity and acceleration is connected with setting parameters of dampers and input seismic waves.

The acceleration responses have obvious difference under different input seismic waves.

Seismic waves traveling between Earth's poles move faster than those moving east-west, and now scientists think they may know why.

When an elephant rumbles , the sound generates seismic waves that travel through the ground.

The first key discovery had to do with (seismic) waves --- remember they are the (vibrations) caused by earthquakes.

These happen as the seismic waves from a mainshock pass through the Earth's crust, which results in transient changes.

Seismic waves from elephant vocalizations: A possible communication mode?

The first key discovery had to do with the seismic waves. Remember, they are the vibrations caused by earthquakes.

The two-dimensional Time-History analysis results are contrasted in the different seismic waves.

For one, any seismic waves that did make their way from Japan to the Chilean coast could play a slight role in ground-shaking.

Based on the theory of magneto-elastic waves, a geomagnetic disturbance accompanying the propagation of seismic waves was studied.

The first key discovery had to do with seismic waves, remember they are the vibrations caused by earth quakes.

Let us now face the problem of the actual mechanical generation of the seismic waves.

Seismic waves traveling north-south were reaching their destinations about 3 percent faster than waves moving along east-west paths.

When this happens, seismic waves travel faster than usual through the rock.

Refers to the super-earthquake seismic waves very strong earthquake.

Seismic waves produced by earthquakes damage buildings and other structures by making them move in various ways.

This first key discovery had to do with seismic waves.

If I'm putting petrol in my car, I don't need to know how to solve the inverse problem for seismic waves.

Under the action of various seismic waves, the rules of structural response are not same with the variation site.

An earthquake is the result from the sudden release of stored energy in the Earth's crust that creates seismic waves.

Scientists assign a magnitude rating to earthquakes based on the strength and duration of their seismic waves.

Seismic sections show the response of the earth to seismic waves.

The underwater earthquake happens and the seismic waves spread out.

There are many seismographic stations in the world, that receive seismic waves generated by earthquakes.

and the elevation has amplification effect on seismic waves totally.

Seismic waves are the fastest way to get information out from the earthquake.

The blasting seismic waves can make the rock mass to be loosened and ruptured, even arouse the sliding failure.

The unusual reflection of seismic waves occurred 1200 meter under the earth.

For example, when rock is stressed it transmits seismic waves at changing speeds.

This is because the seismic waves from the ground came to the ground, vertical landing because of the first wave.

Study of Attenuation Characteristics of the Central and Eastern Tianshan, Xinjiang Using Digital Seismic Waves

Study of basement structure and hydrocarbon reservoir by scattering analysis of seismic waves in Russia

Observation on Effect about Modified Eight Health Restoring Powder Used in Lithotrity of Vitro Seismic Waves

Elasto-plastic response analysis of a complicated shield tunnel system subjected to incident seismic waves

Field Experiment and its Analyses of Attenuation Law for Seismic Waves Resulting from Rock Blasting

Influence of body position changing on pain of patients with urinary system stone undergoing extracorporeal seismic waves stone broken

Numerical Simulation of the Effect of Underwater Blasting Seismic Waves under Different Explosions and Ground Conditions

Modeling research on characteristics and extraction method of abnormal seismic waves on small scale karst collapse column

Propagation characteristics of seismic waves in transverse isotropic medium

Regression Analysis on Attenuation Law of Blasting Seismic Waves at Fuling Ejinggyan Quarry

Transmitting boundary model for periodically spaced structure-foundation systems subject to upgoing seismic waves

Seismic Waves Stimulated in Homogeneous Isotropic and Elastic Medium by Various Seismic Sources

Determination of Seismic Waves Introduced into Bridge Seismic Response Analysis

A nonlinear dynamic analysis of the frame structure and foundation interaction under the action of blasting seismic waves

A Method of Inversion to Enhance the Resolution Power of Superimposed Seismic Waves

Ultrasonic Simulation of Seismic Waves Affected by Mine Water Invasion in North China Coalfield

Experimental Study on Characteristics of Man-made Blasting Caused Seismic Waves

Discrete Particle System Dynamics for Modeling Seismic Waves

Analysis of Shock Characteristic for Explosion Seismic Waves

Numerical Simulation of the Effect of Blasting Seismic Waves on Ground Structure

Inversion of far-field seismic waves at Shidao Seismographic Station

Influences of Porosity and Clay Content on Velocities of Seismic Waves

Analyses of seismic waves for building structure design based on the design code of earthquake-resistant structures

Application of Some Mathematical Methods for Inversion on Seismic Waves

The Fractal Characteristics of Seismic Waves

Safety distance of explosion induced by seismic waves

Analysis on Anti-seismic Properties of Buried Pipelines under the Action of Seismic Waves

CHILE'S SEISMIC WAVES CIRCLED EARTH AND HIT CALIFORNIA

Analysis to First Breaks in Cross Hole Seismic Waves

Summaries of the Research of the Co-seismic Response of Well-Aquifer Systems to Seismic Waves in China