The Rapid Calculation of Potential Anomalies
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ID: 292135
1973
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Abstract
It is shown how a series of Fourier transforms can be used to calculate the magnetic or gravitational anomaly caused by an uneven, non-uniform layer of material. Modern methods for finding Fourier transforms numerically are very fast and make this approach attractive in situations where large quantities of observations are available.
| Reference Key |
openalex_W2150226675
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|---|---|
| Authors | Robert L. Parker |
| Journal | geophysical journal international |
| Year | 1973 |
| DOI |
10.1111/j.1365-246x.1973.tb06513.x
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| URL | |
| Keywords | Keywords not found |
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