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This paper will help to further constrain geodynamic models for the evolution of northern Tibet through two techniques that employ Bouguer gravity anomaly data: the first is isostatic correction of Bouguer gravity anomalies and the second is 2-D density modeling along a profile at 88.5°E from 30°N to 37°N within the Tibetan Plateau. Areas dominated by volcanic rocks exhibit ultra-low Bouguer gravity...
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