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  • In [[reflection seismology]], the '''anelastic attenuation factor''', often expressed as '''seismic qu ...le.<ref>Sheriff, R. E., Geldart, L. P., (1995), 2nd Edition. ''Exploration Seismology''. Cambridge University Press.</ref> ...
    5 KB (798 words) - 18:38, 20 November 2023
  • [[Category:Seismology instruments]] [[Category:Seismology measurement]] ...
    4 KB (602 words) - 21:01, 21 October 2022
  • ...lied to the physical body, such as the atmosphere or the Earth's crust. In seismology or geodesy it describes the effects of the body to applied forcing (tidal a ...p;= 0.01&nbsp;m/s<sup>2</sup> and 1 bar&nbsp;= 100 kPa, so in SI units the measurement would be in units of; ...
    2 KB (354 words) - 09:00, 23 June 2021
  • [[Category:Seismology measurement]] ...
    3 KB (399 words) - 07:38, 3 July 2021
  • ...he attenuation α(w) to be strictly linear with frequency over the range of measurement:<ref>Wang 2008, p. 18, sec. 2.1: Kolsky's attenuation-dispersion model</ref [[Category:Seismology measurement]] ...
    4 KB (559 words) - 01:10, 27 September 2022
  • ...vide a model of the earth's response to [[seismic wave]]s. In [[reflection seismology]], the '''anelastic attenuation factor''', often expressed as '''seismic qu ...uation ''α''(''w'') to be strictly linear with frequency over the range of measurement:<ref>Wang 2008, p. 18, sec. 2.1: Kolsky's attenuation-dispersion model</ref ...
    7 KB (1,100 words) - 07:43, 3 June 2021
  • [[Category:Seismology measurement]] ...
    3 KB (473 words) - 01:28, 8 February 2025
  • '''Dispersive body waves''' is an important aspect of [[Seismology|seismic theory]]. When a wave propagates through subsurface materials both ...on coefficient a(w) is strictly linear in the frequency, over the range of measurement. We can call it bw. (b)The wave motion is linear i.e. the principle of supe ...
    9 KB (1,432 words) - 01:11, 27 September 2022
  • ...he attenuation α(w) to be strictly linear with frequency over the range of measurement:<ref>Wang 2008, p. 18, sec. 2.1: Kolsky's attenuation-dispersion model</ref [[Category:Seismology measurement]] ...
    5 KB (892 words) - 03:48, 28 March 2023
  • ...is a data processing technology for enhancing the resolution of reflection seismology images where the stability of the method used is considered. Q is the [[ane [[Category:Seismology measurement]] ...
    7 KB (1,150 words) - 22:06, 29 February 2024
  • ...Great Neapolitan Earthquake of 1857: The First Principles of Observational Seismology as Developed in the Report to the Royal Society of London of the Expedition |title= Elementary Seismology ...
    11 KB (1,544 words) - 19:52, 29 November 2024
  • ...a data processing technology for enhancing the resolution of [[reflection seismology]] images. Q is the [[anelastic attenuation factor]] or the seismic quality ...he attenuation α(w) to be strictly linear with frequency over the range of measurement:<ref>Wang 2008, p. 18, sec. 2.1: Kolsky's attenuation-dispersion model</ref ...
    10 KB (1,628 words) - 02:49, 4 January 2022
  • ...eismic signals.<ref>J. H. Justice (1985), "Array processing in exploration seismology", in S. Haykin, ed., ''Array Signal Processing'', Englewood Cliffs, New Jer ...eive one desired and {{mvar|M}} undesired broadband interferences. Let the measurement of {{mvar|n}}th sensor be modeled by the expression: ...
    9 KB (1,440 words) - 17:57, 5 February 2025
  • {{Short description|Measurement technique in microwave engineering}} '''Nicolson–Ross–Weir method''' is a [[measurement]] technique for determination of complex [[Permittivity|permittivities]] an ...
    11 KB (1,411 words) - 21:48, 13 September 2024
  • {{Short description|Earthquake measurement scale}} ...s one of the [[Seismic scale#Magnitude scales|magnitude scales]] used in [[seismology]] to describe the size of an [[earthquake]]. It is based on measurements of ...
    7 KB (977 words) - 17:40, 5 February 2025
  • In seismology, surface waves are collected along with other seismic data, but are traditi ...se. The shot gather is modified to minimize the influence of [[Body wave (seismology)|body waves]]. As the data is gathered, the spectral analyzer is able to g ...
    22 KB (3,305 words) - 22:08, 18 May 2022
  • ...acroscopic brittle behavior, such as fracturing, is observed. For accurate measurement, this must be done under several controlled conditions, including but not l ...h the initial and final dimensions of the rock sample. For Elongation, the measurement is a uni-dimensional initial and final length, the former measured before a ...
    12 KB (1,817 words) - 10:17, 1 January 2025
  • ...téphane|last11=Gimbert|first11=Florent|date=2015-05-01|title=Environmental seismology: What can we learn on earth surface processes with ambient noise?|url=https [[Category:Seismology measurement]] ...
    18 KB (2,592 words) - 11:44, 29 January 2025
  • ...eds), ''Modern Approaches in Solid Earth Sciences'' (vol. 2), ''Historical Seismology: Interdisciplinary Studies of Past and Recent Earthquakes,'' Springer, Dord ...{{M|w}}.<ref>{{Harvnb|Richter|1935}}.</ref><ref>Richter, C.F., "Elementary Seismology", ed, Vol., W. H. Freeman and Co., San Francisco, 1956.</ref> The {{M|b}} s ...
    30 KB (4,275 words) - 02:49, 31 January 2025
  • Seismic noise is relevant to any discipline that depends on [[seismology]], including [[geology]], [[oil exploration]], [[hydrology]], and [[earthqu ...]]; [[Natural environment|Environmental]] monitoring, such as in [[fluvial seismology]]; and estimating [[seismic microzonation]] maps to characterize local and ...
    31 KB (4,362 words) - 19:54, 29 November 2024
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