seismic gap - Übersetzung nach russisch
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  3. seismic gap

seismic gap - Übersetzung nach russisch

SEGMENT OF AN ACTIVE FAULT KNOWN TO PRODUCE SIGNIFICANT EARTHQUAKES THAT HAS NOT SLIPPED IN AN UNUSUALLY LONG TIME
Seismic Gap; Seismic gap hypothesis

seismic gap         

нефтегазовая промышленность

область пониженной интенсивности

область разрыва сейсмических границ (на разрезе)

seismic shock         
  • Earthquake wave paths
  • The scheme of motion for spheroidal <sub>0</sub>S<sub>2</sub> oscillation.Dashed lines give nodal (zero) lines. Arrows give the sense of motion.
  • The sense of motion for toroidal <sub>0</sub>T<sub>1</sub> oscillation for two moments of time.
  • The hypocenter/epicenter of an earthquake is calculated by using the seismic data of that earthquake from at least three different locations. The hypocenter/epicenter is found at the intersection of three circles centered on three observation stations, here shown in Japan, Australia and the United States. The radius of each circle is calculated from the difference in the arrival times of P- and S-waves at the corresponding station.
  • s2cid=4304379 }}</ref> The negligible ''S''-wave velocity in the outer core occurs because it is liquid, while in the solid inner core the ''S''-wave velocity is non-zero
  • Patterns of seismic wave travel through Earth’s mantle and core. S-waves can’t travel through the liquid outer core, so they leave a shadow on Earth’s far side. P-waves do travel through the core, but P-wave refraction bends seismic waves away from P-wave shadow zones.
SEISMIC, VOLCANIC, OR EXPLOSIVE ENERGY THAT TRAVELS THROUGH EARTH'S LAYERS
Seismic waves; Earth quake waves; Elastic p-wave; Elastic p wave; Elastic s wave; Elastic s-wave; Elastic P-Wave; Elastic S-Wave; Body wave (seismology); Seismic shock; Body-wave seismograms; Seismic velocity; Seismic Velocity; Seismic graph; Earthquake waves; Seismic energy; Seismic energy waves

нефтегазовая промышленность

сейсмический импульс

seismic waves         
  • Earthquake wave paths
  • The scheme of motion for spheroidal <sub>0</sub>S<sub>2</sub> oscillation.Dashed lines give nodal (zero) lines. Arrows give the sense of motion.
  • The sense of motion for toroidal <sub>0</sub>T<sub>1</sub> oscillation for two moments of time.
  • The hypocenter/epicenter of an earthquake is calculated by using the seismic data of that earthquake from at least three different locations. The hypocenter/epicenter is found at the intersection of three circles centered on three observation stations, here shown in Japan, Australia and the United States. The radius of each circle is calculated from the difference in the arrival times of P- and S-waves at the corresponding station.
  • s2cid=4304379 }}</ref> The negligible ''S''-wave velocity in the outer core occurs because it is liquid, while in the solid inner core the ''S''-wave velocity is non-zero
  • Patterns of seismic wave travel through Earth’s mantle and core. S-waves can’t travel through the liquid outer core, so they leave a shadow on Earth’s far side. P-waves do travel through the core, but P-wave refraction bends seismic waves away from P-wave shadow zones.
SEISMIC, VOLCANIC, OR EXPLOSIVE ENERGY THAT TRAVELS THROUGH EARTH'S LAYERS
Seismic waves; Earth quake waves; Elastic p-wave; Elastic p wave; Elastic s wave; Elastic s-wave; Elastic P-Wave; Elastic S-Wave; Body wave (seismology); Seismic shock; Body-wave seismograms; Seismic velocity; Seismic Velocity; Seismic graph; Earthquake waves; Seismic energy; Seismic energy waves

общая лексика

сейсмические волны

Definition

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Wikipedia

Seismic gap

A seismic gap is a segment of an active fault known to produce significant earthquakes that has not slipped in an unusually long time, compared with other segments along the same structure. There is a hypothesis or theory that states that over long periods of time, the displacement on any segment must be equal to that experienced by all the other parts of the fault. Any large and longstanding gap is, therefore, considered to be the fault segment most likely to suffer future earthquakes.

The applicability of this approach has been criticised by some seismologists although earthquakes sometimes have occurred in previously-identified seismic gaps.

https://en.wikipedia.org/wiki/Seismic gap
Übersetzung von &#39seismic gap&#39 in Russisch
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