Geophysical survey
From Wikipedia, the free encyclopedia
Geophysical survey is the systematic collection of geophysical data for spatial studies. Geophysical surveys may use a great variety of sensing instruments, and data may be collected from above or below the Earth's surface or from aerial or marine platforms. Geophysical surveys have many applications in Earth science, archaeology, mineral and energy exploration, and engineering. Geophysical surveys are used in industry as well as for academic research.
Contents |
[edit] Types of geophysical survey
There are many methods and types of instrumentation used in geophysical surveys. Technologies used for geophysical surveys include:[1]
- Seismic methods, such as reflection seismology, seismic refraction, and seismic tomography.
- Seismoelectrical method
- Geodesy and gravity techniques, including gravimetry and gravity gradiometry.
- Magnetic techniques, including aeromagnetic surveys and magnetometers.
- Electrical techniques, including electrical resistivity tomography, induced polarization and spontaneous potential.
- Electromagnetic methods, such as magnetotellurics, ground penetrating radar and transient/time-domain electromagnetics.
- Borehole geophysics, also called well logging.
- Remote sensing techniques, including hyperspectral.
[edit] See also
[edit] Notes
[edit] References
- Mussett, Alan E.; Khan, M. Aftab (2000). Looking into the Earth: An introduction to geological geophysics. Cambridge University Press. ISBN 0521780853.
- Telford, William Murray; Geldart, L. P.; Sheriff, Robert E. (1990). Applied geophysics. Cambridge University Press. ISBN 9780521339384.
| This geophysics-related article is a stub. You can help Wikipedia by expanding it. |