Spatial Power Spectral Density Distribution of Magnetic Sources in the Gulf of Mexico and Caribbean Plate
A Garcia-Reyes, J Dyment - AGU Fall Meeting Abstracts, 2020 - ui.adsabs.harvard.edu
Spectral methods are widely used in magnetism and gravimetry, including the estimation of
the depth to the centroid of the anomaly source after Spector and Grant (1970). They aim to
decompose the signal to its constitutive sources in the frequency domain. The power
spectral density of a potential field decreases exponentially in function of the depth to the
source and the wavelength. Hence, we usually relate deep sources to strong spectrum at
long wavelength which decays rapidly. However, to estimate the depth to the source is not …
the depth to the centroid of the anomaly source after Spector and Grant (1970). They aim to
decompose the signal to its constitutive sources in the frequency domain. The power
spectral density of a potential field decreases exponentially in function of the depth to the
source and the wavelength. Hence, we usually relate deep sources to strong spectrum at
long wavelength which decays rapidly. However, to estimate the depth to the source is not …
以上显示的是最相近的搜索结果。 查看全部搜索结果