Download scientific diagram | Bouguer gravity map showing the gravity contour used in the flexural modeling on the 2-D transects. from publication: Mapping the deep lithospheric structure beneath the eastern margin of the Tibetan Plateau from gravity anomalies | 1] Various authors have investigated the mechanism of lateral support of the lithosphere in maintaining the uplift of the Tibetan Plateau, based on gravity data and elastic flexural modeling, in the south of the plateau across the Himalayas and in the north and the northwest | Lithosphere, Himalayas and Tibet | ResearchGate, the professional network for scientists.
a) Bouguer gravity anomaly map of the study area. (b) Residual gravity
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Bouguer gravity anomaly map of the study area, contour interval is 10 mGal
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