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  • ...k and forth over only a small portion of the section so that the resulting wave blends with the primary pulse, changing its waveshape and adding a tail. Se
    348 bytes (56 words) - 18:47, 27 April 2017
  • ...es the channel. (<b>e</b>) The high-frequency portion of (d), the <b>water wave</b>; its arrival is used in refraction work to determine the range. (From C
    762 bytes (125 words) - 21:45, 19 June 2017
  • ...es the channel. (<b>e</b>) The high-frequency portion of (d), the <b>water wave</b>; its arrival is used in refraction work to determine the range. (From C
    800 bytes (130 words) - 10:31, 11 July 2017
  • ...r investigating the factors affecting the amplitude of a returning seismic wave when the angle of incidence is altered - also known as [[Special:MyLanguage
    799 bytes (114 words) - 06:08, 22 October 2017
  • ...es are generated: reflected P-wave and S-wave and transmitted P-wave and S-wave. The partition of energy among these is found from four boundary conditions
    559 bytes (86 words) - 06:08, 22 October 2017
  • {{#category_index:S|standing wave}} ...length intervals. Continuous-wave radio-navigation systems set up standing-wave patterns.
    495 bytes (66 words) - 05:30, 1 November 2017
  • ...eflector mainly effective in generating a reflection since, for a harmonic wave, the effects of successive zones generally cancel each other. A nomogram fo
    1 KB (195 words) - 10:32, 21 November 2017
  • ...the first arrival of the downgoing wave is time-coincident with an upgoing wave.&#x2019;&#x2019;
    522 bytes (83 words) - 12:16, 7 March 2017
  • ...f layers 1, 2, and ''V''<sub>''S''1</sub>, ''V''<sub>''S''2</sub> is the S-wave velocity in layers 1, 2.
    277 bytes (44 words) - 13:33, 19 February 2017
  • ...cuum, 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.
    233 bytes (40 words) - 14:54, 29 January 2017
  • ...2</b>. Seismic wave energy falling on a reflector and thus available to be reflected. It depends on source-receiver configuration and velocity distribution, esp
    454 bytes (62 words) - 23:22, 18 January 2017
  • ...ath (for example, by an overhanging salt flank), it is called a <b>turning-wave reflection</b> (see Figure [[Special:MyLanguage/Dictionary:Fig_D-19|D-19]])
    519 bytes (86 words) - 15:26, 9 April 2019
  • ...ath (for example, by an overhanging salt flank), it is called a <b>turning-wave reflection</b> (see Figure [[Special:MyLanguage/Dictionary:Fig_D-19|D-19]])
    519 bytes (86 words) - 07:31, 19 March 2018
  • ...e picked with reasonable certainty. Depends on the energy of the reflected wave, the presence of noise, and the processing to which the data are subjected
    463 bytes (69 words) - 08:59, 26 March 2018
  • ...es the channel. (<b>e</b>) The high-frequency portion of (d), the <b>water wave</b>; its arrival is used in refraction work to determine the range. (From C
    762 bytes (125 words) - 08:55, 28 March 2018
  • This model is a consequence of the concept that each reflected wave causes its own effect at each geophone (or hydrophone) independent of what
    447 bytes (72 words) - 09:33, 28 March 2018
  • ...l&#x2202; nat&#x2019; ik) The locus for a given traveltime of wave energy reflected or refracted at a surface. Wavefronts are aplanatic surfaces for reflection
    821 bytes (118 words) - 09:45, 28 March 2018
  • <b>1</b>. Head-wave energy that has been reflected or diffracted back from a discontinuity in a refractor, such as a fault. Se
    147 bytes (27 words) - 09:59, 28 March 2018
  • .... A refraction multiple, involving head-wave energy that has been multiply reflected between reflectors. The extra travel may occur at any time during the trave
    304 bytes (48 words) - 09:59, 28 March 2018
  • The energy or wave from a seismic source that has been reflected (returned) from an acoustic-impedance contrast (<b>reflector</b>) or series
    558 bytes (79 words) - 10:07, 28 March 2018

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