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  2. Reflection seismology - Wikipedia

    en.wikipedia.org/wiki/Reflection_seismology

    This method can be known as life of field seismic (LoFS) or permanent reservoir monitoring (PRM). [36] 4D seismic surveys using towed streamer technology can be very challenging as the aim of a 4D survey it to repeat the original or baseline survey as accurately as possible.

  3. Seismic data acquisition - Wikipedia

    en.wikipedia.org/wiki/Seismic_data_acquisition

    For land acquisition, different types of sources may be used depending on the acquisition settings. Explosive sources such as dynamite are the preferred seismic sources in rough terrains, in areas with high topographic variability or in environmentally sensitive areas e.g. marshes, farming fields, mountainous regions etc. [4] Such type of sources needs to be buried (coupled) into the ground in ...

  4. Seismic velocity structure - Wikipedia

    en.wikipedia.org/wiki/Seismic_Velocity_Structure

    By analysing seismic waves generated by earthquakes, the velocity structure can be studied which can reflect the subsurface condition where the seismic wave propagated. Receiver Function Analysis Receiver function analysis is a seismic method that interprets waveform data to study the conversions and reflections of seismic waves at subsurface ...

  5. Seismology - Wikipedia

    en.wikipedia.org/wiki/Seismology

    Seismology (/ s aɪ z ˈ m ɒ l ə dʒ i, s aɪ s-/; from Ancient Greek σεισμός (seismós) meaning "earthquake" and -λογία (-logía) meaning "study of") is the scientific study of earthquakes (or generally, quakes) and the generation and propagation of elastic waves through planetary bodies.

  6. Fault trace - Wikipedia

    en.wikipedia.org/wiki/Fault_trace

    Along the Motagua Fault trace (1976 Guatemala earthquake) where it crosses the Gualán soccer field. This zigzag type of fault trace is known as "mole track", which is best developed in hard-packed, brittle surface materials. The San Andreas fault trace runs along the base of the Temblor Range of mountains near Bakersfield, California. (The ...

  7. Near-surface geophysics - Wikipedia

    en.wikipedia.org/wiki/Near-surface_geophysics

    Upper figure: a seismic profile showing intensity vs round-trip travel time. Lower figure: an interpretation of the results. Seismology makes use of the ability of vibrations to travel through rock as seismic waves. These waves come in two types: pressure waves and shear waves . P-waves travel faster than S-waves, and both have trajectories ...

  8. Exploration geophysics - Wikipedia

    en.wikipedia.org/wiki/Exploration_geophysics

    Exploration geophysics is an applied branch of geophysics and economic geology, which uses physical methods at the surface of the Earth, such as seismic, gravitational, magnetic, electrical and electromagnetic, to measure the physical properties of the subsurface, along with the anomalies in those properties.

  9. Isoseismal map - Wikipedia

    en.wikipedia.org/wiki/Isoseismal_map

    Isoseismal map for the 1968 Illinois earthquake. In seismology, an isoseismal map is used to show countour lines of equally felt seismic intensity, generally measured on the Modified Mercalli scale. Such maps help to identify earthquake epicenters, particularly where no instrumental records exist, such as for historical earthquakes.