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An analytic signal approach to the interpretation of total field magnetic anomalies 1
Author(s) -
Qin Shuang
Publication year - 1994
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1111/j.1365-2478.1994.tb00234.x
Subject(s) - interpretation (philosophy) , magnetization , magnetic field , field (mathematics) , magnetic anomaly , analytic signal , square root , signal (programming language) , physics , directional derivative , potential field , nuclear magnetic resonance , geology , mathematics , geophysics , geometry , computer science , signal processing , quantum mechanics , pure mathematics , telecommunications , radar , programming language
The analytic signal (AS) is defined as the square root of the sum of the squares of the vertical and the two horizontal derivatives of the total magnetic field Δ T. This paper verifies theoretically that peaks of the AS correlate directly with their magnetic causative bodies and are positioned symmetrically over them, i.e. the main feature of the AS is that it is independent of the inclination of the magnetic field. This avoids the difficulties that are often faced in the conventional process of reduction to pole for Δ T , when the direction of magnetization of the causative bodies is not known. In addition, the AS has characteristics similar to the derivative features of the magnetic field, so that it is very sensitive to edge effects of the causative magnetic bodies. The theoretical derivations are tested by comparison with calculations on models, and, in a field example from Hunan Province, China, the AS is applied successfully to the interpretation of Δ T , whereas the conventional process of reduction to pole fails, due to the reverse magnetization of the causative body.