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Deep-seated lithospheric folding can be revealed using a method that combines gravity inversion calculations and isostatic analyses.The determination of the crustal structure is essential in geophysics, as it gives insight into the geohistory, tectonic environment, geohazard mitigation, etc. Here we present the latest advance on three-dimensional modeling representing the Tibetan Mohorovičić discontinuity (topography and ranges) and its deformation (fold), revealed by analyzing gravity data from GOCE mission

Estimating the 3D fold structure of the crust–mantle boundary