The Bouguer gravity anomaly in the southwest basin has an obvious trend distributed in a NE direction. 4 Methods 4.1 Improved method for Moho recovery The spatial-domain gravity inversion method was adopted for the estimation of Moho depth, (1) Φ ( p ) = [ d obs − d ( p ) ] T [ d obs − d ( p ) ] where d obs is the observation data vector; d ( p ) is the predicted data vector.
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Depth distribution of Moho model and tectonic patterns in South China Sea and adjacent areas.
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