amplitude variation with offset - translation to ρωσικά
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amplitude variation with offset - translation to ρωσικά

TERM FOR REFERRING TO THE DEPENDENCY OF THE SEISMIC ATTRIBUTE, AMPLITUDE, WITH THE DISTANCE BETWEEN THE SOURCE AND RECEIVER
Amplitude Variation with Offset; Amplitude Versus Offset; Amplitude variation with offset
  • Diagram showing how the layout of sources and receivers affects the angle of incidence
  • Diagram showing how to construct an AVO [[Cross-plot]]
  • Diagram showing the mode conversions that occur when a P-wave reflects off an interface at non-normal incidence

amplitude variation with offset         

сейсмология

амплитуда как функция удаления

amplitude versus offset         
амплитуда как функция удаления
variation         
WIKIMEDIA DISAMBIGUATION PAGE
Variations; Varied; Varying; Variation (disambiguation); Viccitude; Variations (album); Variation (combinatorics); Variations (Combinatorics); Variation (Combinatorics)

[ve(ə)ri'eiʃ(ə)n]

общая лексика

вариация

изменчивость

изменение

вариационный

варьирование

колебание

колебательность

магнитное склонение

неравномерность

отклонение

разновидность

ход зависимости

нефтегазовая промышленность

отклонение (от номинальной величины)

Смотрите также

age variation; autogenous variation; balanced variation; brusque variation; bud variation; chance variation; continuous variation; cryptic variation; determinate variation; directional variation; discontinuous variation; discrete variation; ecological variation; environmental variation; food variations; genetic variation; geographic variation; group variation; homologous variation; host controlled variation; idiotypic variation; individual variation; interspecific variation; intrapopulation variation; intraspecific variation; local variation; phase variation; phenotypic variation; remaining variation; seasonal variation; sex-associated variation; somatic variation; somatogenic variation; stimulus parameter variation; absolute variation; admissible variation; amount of variation; aperiodic variation; batch variation; batch-to-batch variation; boundary variation; bounded variation; coefficient of variation; combined variation; component of variation; constant of variation; constrained variation; controllable variation; daily variation; day-to-day variation; direct variation; domain of variation; dominated variation; downward variation; explained variation; finite variation; first variation; fractional variation; free variation; generalized variation; gross variation; harmonic variation; higher-order variation; infinitesimal variation; intermittent variation; inverse variation; joint variation; law of variation; limited variation; limits of variation; long-period variation; lower variation; measure variation; mixed variation; n-parameter variation; needle-shaped variation; negative variation; net variation; nonlinear variation; nonperiodic variation; normal variation; one-sided variation; overall variation; pitch variation; plane variation; positive variation; quadratic variation; random variation; region of variation; regular variation; relative variation; saltatory variation; sampling variation; second variation; secular variation; short-period variation; significant variation; smooth variation; source of variation; strong variation; systematic variation; time variation; total variation; transient variation; type of variation; unbounded variation; uncontrolled variation; unexplained variation; unfree variation; upper variation; variation diminishing matrix; variation estimation; variation factor; variation interval; variation kernel; variation limiting matrix; variation measure; variation norm; variation of constants; variation of curve; variation of function; variation of functional; variation of parameters; variation of sign; variation range; weak variation; variations from plumb; variation in the magnitude; variation in the sense; variations in the shape; variation with time; variation of the bending moment along the length of the beam; variation of the project; color variations; diurnal variation; magnetic variation; probable variations in dead load during construction; stress variation; temperature variations; variation of reflection amplitude with angle of incidence; variation of reflection amplitude with offset; variation of reflection coefficient with angle of incidence; amplitude variation with offset; layer thickness variation; near-surface velocity variations; penetration rate variation; reliability variation; rock permeability variations; strength variation; weathering variation; weathering velocity variation; weight-on-bit variation

существительное

общая лексика

изменение

перемена

варьирование

колебание

разновидность

вариант

отклонение

изменение, перемена

склонение магнитной стрелки

специальный термин

вариация

физика

магнитное склонение

грамматика

флексия

биология

аберрация

генетическая изменчивость

мутация

Ορισμός

variation
¦ noun
1. a change or slight difference in condition, amount, or level.
(also magnetic variation) the angular difference between true north and magnetic north at a particular place.
2. a different or distinct form or version.
Music a new but still recognizable version of a theme.
Ballet a solo dance as part of a performance.
Derivatives
variational adjective

Βικιπαίδεια

Amplitude versus offset

In geophysics and reflection seismology, amplitude versus offset (AVO) or amplitude variation with offset is the general term for referring to the dependency of the seismic attribute, amplitude, with the distance between the source and receiver (the offset). AVO analysis is a technique that geophysicists can execute on seismic data to determine a rock's fluid content, porosity, density or seismic velocity, shear wave information, fluid indicators (hydrocarbon indications).

The phenomenon is based on the relationship between the reflection coefficient and the angle of incidence and has been understood since the early 20th century when Karl Zoeppritz wrote down the Zoeppritz equations. Due to its physical origin, AVO can also be known as amplitude versus angle (AVA), but AVO is the more commonly used term because the offset is what a geophysicist can vary in order to change the angle of incidence. (See diagram)

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