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Alternative gravimetric methodology for isostatic analyses An example for Bolivian Andes

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Academic year: 2020

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Figure 1. A: Location of the studied area in Bolivia. B: Tectonomorphic units of the Andean chain.
Figure 2. A: Topographic contours for Bolivia from GLOBE digital elevation model (contour interval 1000 m)
Figure 3. A: Geoid undulations derived from EGM96 geopotential model (contour interval 5 m)
Figure 4. A: Residual geoid undulations for the studied area obtained through the sparse Fourier transform method (contour interval 2 m)
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