Disruptive bodies

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In geophysics and potential theory, a disruptive body is a body that causes irregularities in the earth's gravitational or magnetic field .

Disruptive bodies stand out from their surroundings by at least one clearly different rock parameter, in particular:

They can be of purely scientific interest (such as the Ivrea body for geoid determination in Switzerland) or have economic importance as a deposit - e.g. B. Ores , special rocks such as kaolin or serpentine , petroleum -höffige layers or construction and bulk raw materials .

Normal field, anomaly and interference potential

The difference to the surrounding rock can be determined by precise measurements in a force field over relatively large distances by comparing the measured field (e.g. gravity ) with its normal field typical for the respective region . The difference is called an anomaly ( magnetic or gravity anomaly ) and is represented graphically or digitally in the form of so-called isanomal maps. The location and structure of the disruptive body can then be deduced from the local course of these anomalies.

The exact mathematical-physical analysis of the anomaly field is carried out with the help of the interference potential or the potential-theoretical divergence , for which there are a number of approximation methods. Because in general neither the location of the disruptive body nor the calculation of its properties is clear; one must first adopt approximate values ​​and gradually adapt them to the measurements by making targeted changes to the modeling (“ trial and error ”). In most cases, additional data from geology , for example, are required (e.g. on outcrops , observed faults or crevices , edges of sedimentary basins , etc.) in order to be able to narrow down the location of the disruptive body sought.

Other meanings of the term "disruptive body"

See also