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  2. Reflection seismology - Wikipedia

    en.wikipedia.org/wiki/Reflection_seismology

    Download as PDF; Printable version; ... (or seismic reflection) ... the seismic technique explored the possibility of full three-dimensional acquisition and ...

  3. SEG-Y - Wikipedia

    en.wikipedia.org/wiki/SEG-Y

    SEG-Y Files are stored in a hierarchical byte-stream format that combines both textual and binary data segments. The following chart shows the byte stream structure of revision 1 (2002), [5] with revision 2 (2017) only adding an optional data trailer for 1 or more 3200-byte records at the end: [6] [7]

  4. Amplitude versus offset - Wikipedia

    en.wikipedia.org/wiki/Amplitude_versus_offset

    Modern seismic reflection surveys are designed and acquired in such a way that the same point on the subsurface is sampled multiple times, with each sample having a different source and receiver location. The seismic data is then carefully processed to preserve seismic amplitudes and accurately determine the spatial coordinates of each sample.

  5. J. Clarence Karcher - Wikipedia

    en.wikipedia.org/wiki/J._Clarence_Karcher

    On June 4, 1971, the Geophysical Society of Oklahoma city erected a monument in the front lawn of Belle Isle Library, recording how in 1921 Karcher and his team recorded their first seismic data, and "proved the validity of the reflection seismograph as a useful tool in the search for oil." [9]

  6. Seismic wide-angle reflection and refraction - Wikipedia

    en.wikipedia.org/wiki/Seismic_wide-angle...

    In comparison to the typical seismic reflection survey, which is restricted to relatively small incidence angles due to the limited offsets between source and receiver, wide-angle reflection and refraction (WARR) data are acquired with long offsets, allowing the recording of both refracted and wide-angle reflection arrivals. [1] [2]

  7. Geophysical survey - Wikipedia

    en.wikipedia.org/wiki/Geophysical_survey

    Seismic methods, such as reflection seismology, seismic refraction, and seismic tomography. This type of survey is carried out to discover the detailed structure of the rock formations beneath the surface of the Earth. Seismoelectrical method; Geodesy and gravity techniques, including gravimetry and gravity gradiometry. This type of survey is ...

  8. Normal moveout - Wikipedia

    en.wikipedia.org/wiki/Normal_moveout

    Seismic data is sorted by common midpoint and then corrected for normal moveout. In reflection seismology, normal moveout (NMO) describes the effect that the distance between a seismic source and a receiver (the offset) has on the arrival time of a reflection in the form of an increase of time with offset. [1]

  9. Synthetic seismogram - Wikipedia

    en.wikipedia.org/wiki/Synthetic_seismogram

    A synthetic seismogram is the result of forward modelling the seismic response of an input earth model, which is defined in terms of 1D, 2D or 3D variations in physical properties. In hydrocarbon exploration this is used to provide a 'tie' between changes in rock properties in a borehole and seismic reflection data at the same location. It can ...