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  • {{#category_index:S|seismic wave}} ...astic disturbance that is propagated from point to point through a medium. Seismic waves are of several types: (a) two types of ''body waves'': ''P-waves'' an
    643 bytes (89 words) - 11:43, 29 April 2017
  • {{#category_index:S|seismic wave}} ...astic disturbance that is propagated from point to point through a medium. Seismic waves are of several types: (a) two types of ''body waves'': ''P-waves'' an
    584 bytes (83 words) - 11:43, 29 April 2017
  • 551 bytes (90 words) - 17:50, 16 November 2019
  • | align="center" | [[Potential functions used to solve wave equations]] * [[Magnitude of disturbance from a seismic source]]
    5 KB (546 words) - 11:21, 14 February 2019

Page text matches

  • ...ge as 0.5 dB/cycle.<ref>Tokso¨z, M. N. and Johnston, D. H., 1982, Seismic wave attenuation: Soc. Expl. Geophys.</ref>
    2 KB (240 words) - 10:39, 17 October 2016
  • ...reflection coefficients'']] (q.v.) at normal incidence, that is, seismic P-wave velocity multiplied by density. Because reflection coefficients change with
    509 bytes (66 words) - 18:28, 28 September 2016
  • {{#category_index:A|acoustic wave}} ...n distinct arrivals. <b>3</b>. More generally, any elastic wave or seismic wave.
    1 KB (176 words) - 10:19, 8 December 2017
  • {{#category_index:A|admittance (seismic)}} ...x2019; when discussing the transfer of energy from a source into a seismic wave.
    383 bytes (55 words) - 14:02, 23 January 2018
  • ...y makes clear which is meant. P-wave anisotropy is usually meant, unless S-wave anisotropy is specified, but anisotropy of P-waves usually implies anisotro ...e=A review of wave motion in anisotropic and cracked elastic-media|journal=Wave Motion|volume=3|issue=4|year=1981|pages=343–391|issn=01652125|doi=10.1016
    12 KB (1,710 words) - 07:26, 14 May 2019
  • {{#category_index:A|array (seismic)}} <b>1</b>. A group of geophones or other seismic receivers connected to a single recording channel <b>(geophone array)</b> o
    3 KB (430 words) - 11:18, 22 January 2018
  • {{#category_index:A|Array Seismic Imager}} ...agnetically clamped 3-component phones. Yields the velocities of different wave modes. A Schlumberger tool.
    286 bytes (38 words) - 14:22, 26 January 2018
  • {{#category_index:A|array sonic/seismic log}} ...lysis of several waves. Schlumberger trade name; Halliburton&#x2019;s Full Wave Sonic System is similar.
    338 bytes (46 words) - 16:47, 28 January 2018
  • .... Calculating the anisotropic elastic parameters that characterize seismic-wave propagation at low frequencies in a layered medium.
    456 bytes (54 words) - 07:25, 24 January 2017
  • ...ree wave types: P- and S-waves and a Biot slow wave. The slow wave couples wave motion to fluid diffusion and propagates at velocities&#x2248;10&#x0020;m/s
    534 bytes (74 words) - 11:04, 24 March 2017
  • ...'', and [[Special:MyLanguage/Dictionary:anisotropy_(seismic)|''anisotropy (seismic)'']].
    2 KB (225 words) - 22:06, 24 March 2017
  • ...surrounding medium. Used to increase the sharpness of a downward-traveling wave and to reduce ghosting.
    566 bytes (82 words) - 21:36, 13 April 2017
  • ...Special:MyLanguage/Dictionary:Fig_R-5|R-5]]). Various arrangements such as wave-shape kits are used to attenuate bubble effects or (as with Maxipulse) to c
    2 KB (233 words) - 21:44, 13 April 2017
  • ...a vacuum, 2.997 925&#x00D7;10<sup>8</sup>&#x0020;m/s. <b>3</b>. A seismic wave reflected at the Earth&#x2019;s mantle-core boundary.
    320 bytes (48 words) - 13:54, 29 January 2017
  • ...y gets trapped; see [[Special:MyLanguage/Dictionary:channel_wave|''channel wave'']]. <b>8</b>. A gate with upper and lower energy thresholds followed by a
    2 KB (252 words) - 09:31, 11 July 2017
  • {{#category_index:C|circumferential wave}} Seismic wave that travels parallel to the Earth&#x2019;s surface.
    195 bytes (24 words) - 17:23, 25 January 2017
  • ...ttering, etc. <b>2</b>. The trailing waveshape that follows the onset of a wave arrival.
    329 bytes (45 words) - 12:03, 27 January 2017
  • {{#category_index:C|converted wave}} Seismic energy that has traveled partly as a P-wave and partly as an S-wave, being converted from one to the other upon reflection or refraction at obl
    3 KB (419 words) - 10:37, 13 November 2017
  • The concept that a seismic trace ''f''(''t'') can be represented by the convolution of an embedded (eq ...ion effects such as absorption. The convolutional model is implied in most seismic processing and interpretation.
    863 bytes (134 words) - 11:52, 4 December 2017
  • ...upt change of slope. Also called <b>break frequency</b>. (b) For a seismic wave generated by an earthquake, the frequency at which the spectral field begin
    430 bytes (67 words) - 11:07, 8 December 2017

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