Gravity and magnetic signals are usually affected by noise, which is in tur
n related either to the geological heterogeneity of the shallow structures
or to the measurement and data processing procedures. Along the map, the si
gnal is represented by field anomalies which overlap with the noise in a va
riable and complicated way. Classical filtering techniques such as the Four
ier (band-pass) filtering or the wavelet "cycle-spinning" method denoise th
e data only in a global sense and are therefore inaccurate when the frequen
cy content of the signal is no longer uniform. We propose instead a localiz
ed denoising of such data, based on localized filtering techniques using th
e wavelet transform. The localized denoising filtering is based on a "soft
thresholding" rule and is characterized by a local thresholding parameter (
LTP). An adaptive tuning of the LTP parameter allows enhancement of the hig
h frequencies of the signal and is effective to remove the noise as much as
possible. The method is confronted using two different kinds of wavelets,
namely the biorthogonal and the multiscale shiftable transforms and is appl
ied to the noisy Vertical derivative of the gravity field of Sicily. The te
chnique proves to be superior to classical methods and may be similarly app
lied to any manner of geophysical data.