azimuthal vertical seismic profiling - translation to russian
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azimuthal vertical seismic profiling - translation to russian

Geographical profiling; Geographic Profiling

azimuthal vertical seismic profiling      

нефтегазовая промышленность

азимутальное вертикальное сейсмическое профилирование

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

vertical
1.
Something that is vertical stands or points straight up.
The gadget can be attached to any vertical or near vertical surface.
? horizontal
ADJ
vertically
Cut each bulb in half vertically.
ADV: ADV after v
2.
The vertical is the direction that points straight up, at an angle of 90 degrees to a flat surface.
Pluto seems to have suffered a major collision that tipped it 122 degrees from the vertical.
N-SING: the N

Wikipedia

Geographic profiling

Geographic profiling is a criminal investigative methodology that analyzes the locations of a connected series of crimes to determine the most probable area of offender residence. By incorporating both qualitative and quantitative methods, it assists in understanding spatial behaviour of an offender and focusing the investigation to a smaller area of the community. Typically used in cases of serial murder or rape (but also arson, bombing, robbery, terrorism and other crimes), the technique helps police detectives prioritize information in large-scale major crime investigations that often involve hundreds or thousands of suspects and tips.

In addition to determining the offender's most likely area of residence, an understanding of the spatial pattern of a crime series and the characteristics of the crime sites can tell investigators other useful information, such as whether the crime was opportunistic and the degree of offender familiarity with the crime location. This is based on the connection between an offender's behavior and his or her non-criminal life.

Geographic profiling is growing in popularity and, combined with offender profiling, can be a helpful tool in the investigation of serial crime.

What is the Russian for azimuthal vertical seismic profiling? Translation of &#39azimuthal vertical