Magnetic Surveying and Anomalies Flashcards
The expected value of the field at any place is taken to be that of the
International Geomagnetic Reference Field (IGRF)
- The difference between the observed and expected values is a magnetic anomaly
Magnetic Anomaly
In land surveying, a portable magnetometer is used to measure the Earth’s surface magnetic field at grid points over a suspected geological structure
Though slow, this method yields a detailed pattern of the magnetic field anomaly due to close proximity measurements to the source
Land Surveying
- Proton-precession magnetometers are most commonly used in
Land Surveying
2 ways of Airborne Magnetic Surveying
- the magnetometer may be mounted rigidly on the airplane at the end of a boom (“bird”)
- towed in an aerodynamic housing behind the plane
magnetometer must be towed some distance d behind the ship to escape its magnetic field
Shipborne Surveying
- proton-precession magnetometer mounted in a waterproof “fish” is towed behind the ship at the end of a long cable
Shipborn Surveying
consists of a pair of alkali-vapor magnetometers maintained at a fixed distance from each other
Magnetic gradiometers
- includes parallel measurement lines and orthogonal cross-tie lines
The Survey Pattern
- variation in intensity of the geomagnetic field at the Earth’s surface during the course of a day
Diurnal Variation
Magnetic anomaly of an inclined magnetization
When an infinitely long dike is magnetized obliquely, its
anomaly can be modeled using __________
inclined dipole or pole distributions