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  • ...listed on this page. All of the data posted on the Open Data page is free and available to the public. For some uses, you may have to request permission ...and geophysical consortia|this page]] for internet-accessible exploration and geophysical consortia.
    42 KB (6,465 words) - 18:07, 15 September 2021
  • Return to [[SEG Honors and Awards]]. ...sukioka]], [[Shinobu Omika]], [[Takeshi Yoshiume]], [[Masashi Mochizuki]], and [[Kenji Uehira]]
    23 KB (2,964 words) - 01:55, 29 September 2019
  • academic authorities on rock physics. He applies rock processes in the Earth’s crust and lithosphere, a major thrust
    10 KB (1,547 words) - 16:37, 25 April 2017
  • ...function of depth based on downhole measurement using logging tools. Here, velocities were measured between the 1000- to 5400-ft depth interval at 2-ft intervals ...le and sand. Porosity changes also can affect interval velocities within a rock layer. Note that well-log measurements have a limited accuracy; therefore,
    11 KB (1,590 words) - 08:01, 18 September 2014
  • ...mptions in estimating [[Dictionary:Acoustic_impedance|acoustic impedance]] and [[Dictionary:AVO|AVO]] attributes. ...acilitate the forthcoming discussion on the link between elastic waves and rock properties, first, we summarize the definitions of [[Mathematical_foundatio
    18 KB (2,723 words) - 16:28, 6 October 2014
  • ...n of wave propagation in elastic solids are derived by using Hooke’s law and Newton’s second law of motion. We shall begin with the stress-strain rela ...components. A normal stress component is ''tensional'' if it is positive, and ''compressional'' if it is negative. To retain the solid volume depicted in
    84 KB (13,083 words) - 11:58, 12 September 2020
  • ...eophysicists is a history of the people who created exploration geophysics and the technologies that they ...technical program with 993 papers presented—589 oral, 119 paper posters, and 285 e-posters.===
    162 KB (23,950 words) - 11:27, 20 June 2016
  • ...omaly is a function of Reflection Amplitude and its controls of Pore fluid and Lithology. A Fizz Gas amplitude anomaly is created when there is a change i ...ed. The ‘Fizz Gas” or low saturations of gas remain in the rock layers and brighten up the Amplitude in a DHI. The amplitude anomalies or bright spots
    5 KB (723 words) - 23:07, 22 July 2018
  • ...material resists change in volume (compression) when subjected to uniform pressure. it is also known as '''Bulk Modulus''' . ...e ratio of the applied pressure(stress) to the volume strain caused by the pressure. This is illustrated below:
    1 KB (175 words) - 15:57, 16 June 2020
  • ...me = Digital Imaging and Deconvolution: The ABCs of Seismic Exploration and Processing ...tle = Digital Imaging and Deconvolution: The ABCs of Seismic Exploration and Processing
    10 KB (1,472 words) - 10:23, 4 May 2021
  • ...me = Digital Imaging and Deconvolution: The ABCs of Seismic Exploration and Processing ...tle = Digital Imaging and Deconvolution: The ABCs of Seismic Exploration and Processing
    10 KB (1,390 words) - 10:24, 4 May 2021
  • ...me = Digital Imaging and Deconvolution: The ABCs of Seismic Exploration and Processing ...tle = Digital Imaging and Deconvolution: The ABCs of Seismic Exploration and Processing
    10 KB (1,402 words) - 16:45, 7 May 2021