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Gravity-Geological Method for Seafloor Topography Inversion Considering Spatial Heterogeneity
Abstract Seafloor topography is highly important in marine science as a crucial physical background field. Seafloor topography inversion mainly relies on marine gravity data to supplement missing bathymetry data in areas lacking ship measurements. However, existing inversion algorithms often overlook the geophysical properties and spatial differences of seafloor topography.
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