Published online by Cambridge University Press: 28 September 2023
Spectral techniques have provided a powerful new tool with which to quantitatively evaluate the state of isostasy at Earth’s bathymetric or topographic features. These techniques can be used to determine information on isostasy directly from observed gravity anomaly and bathymetry or topography data (inverse modelling), as well as to calculate the gravity anomaly from bathymetry or topography data for different isostatic models (forward modelling).
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