Results 141 to 150 of about 107,236 (205)
Crustal velocity structure for Northern Egypt using ambient noise tomography. [PDF]
Sci RepAdam HAA +3 more
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Dataset of Potential Tsunami Scenarios in the South China Sea. [PDF]
Sci DataZhao G, Niu X.
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Subsurface geophysical profiling in Awash Melkesa: Insights into lithology and resource potential. [PDF]
PLoS OneDessalew EA, Mamo T, Ali MY.
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Low-angle subduction of the Indian plate and megathrust geometry below the Eastern Himalayas. [PDF]
Natl Sci RevBai L +6 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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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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GEOPHYSICS, 1950
Speculations are made regarding the significance of the well‐known observation that seismic reflection energy is usually in the frequency range of from 20 to 100 cycles per second. The general absence of reflected energy below 20 cps is attributed to the fact that the wavelengths of seismic waves in this frequency range are becoming large compared to ...
D. H. Clewell, R. F. Simon
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Speculations are made regarding the significance of the well‐known observation that seismic reflection energy is usually in the frequency range of from 20 to 100 cycles per second. The general absence of reflected energy below 20 cps is attributed to the fact that the wavelengths of seismic waves in this frequency range are becoming large compared to ...
D. H. Clewell, R. F. Simon
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1983
Seismic wave propagation is founded on the principles and laws of classical physics: Hooke’s law relating stress and strain, the theory of elasticity, the principles of conservation of energy and momentum, Newton’s laws of motion, and the wave equation.
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Seismic wave propagation is founded on the principles and laws of classical physics: Hooke’s law relating stress and strain, the theory of elasticity, the principles of conservation of energy and momentum, Newton’s laws of motion, and the wave equation.
openaire +1 more source