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  2. SEG-Y - Wikipedia

    en.wikipedia.org/wiki/SEG-Y

    Even before the SEG-Y standard was agreed and published, earlier seismic data format standards published by the SEG such as SEG-A, SEG-B and SEG-C were modified by seismic acquisition companies, though not to the wide extent that the SEG-Y format has been modified by seismic acquisition and processing companies and oil companies using their own ...

  3. Reflection seismology - Wikipedia

    en.wikipedia.org/wiki/Reflection_seismology

    Reflection seismology, more commonly referred to as "seismic reflection" or abbreviated to "seismic" within the hydrocarbon industry, is used by petroleum geologists and geophysicists to map and interpret potential petroleum reservoirs. The size and scale of seismic surveys has increased alongside the significant increases in computer power ...

  4. Bottom simulating reflector - Wikipedia

    en.wikipedia.org/wiki/Bottom_simulating_reflector

    Bottom simulating reflectors (BSRs) are, on seismic reflection profiles, shallow seismic reflection events, characterized by their reflection geometry similar to seafloor bathymetry. [1]. They have, however, the opposite reflection polarity to the seabed reflection, [1] and frequently intersect the primary reflections. [2]

  5. Seismic velocity structure - Wikipedia

    en.wikipedia.org/wiki/Seismic_Velocity_Structure

    Seismic reflection capitalizes on the echo of seismic waves off boundaries where acoustic impedance varies between earth layers. [81] By recording the differences in travel time and wave amplitude, researchers correlate these measurements with subsurface properties to map out velocity structures, akin to seismic refraction but focusing on wave ...

  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. RadExPro seismic software - Wikipedia

    en.wikipedia.org/wiki/RadExPro_seismic_software

    RadExPro is a Windows-based seismic processing software system produced by RadExPro Seismic Software LLC based in Georgia. It is suitable for in-field QC (both online and offline) and processing of 3D and 2D marine and on-land seismic data, advanced processing of HR/UHR offshore seismic, [1] as well as for the onshore near-surface seismic reflection, refraction, MASW, and VSP processing.

  8. 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 ...

  9. 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]