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What is Moho Recovery in Tibet Using Gravity Data about?

This study presents a regional gravimetric method for recovering the Moho depth under the Tibet Plateau, addressing inaccuracies in existing models due to sparse seismic data. By utilizing gravitational potential data from satellite global models, the authors propose a more generic approach that combines gravity data with a functional relationship to interpolate Moho information. The results indicate a difference of about 5 km compared to the CRUST1.0 seismic model, highlighting the effectiveness of the gra

Author

KAMTO Paul

Language

EN