Due to the complexity and overlap effects of gravity anomalies, the gravity high point always deviates from the real position of the target. Researching the offset characteristics is helpful to determine the right location of gravity anomalies. In this paper, a series of forward models were designed to calculate the offset features under different assumptions. Different density models were established based on the measured gravity data in north China Sunhu area and a variety of methods were tried to eliminate offset effects under different conditions. The results indicate that the gravity anomalies of different density bodies can be separated effectively and the real position of target can be correctly located by using the “layer stripping method”.
Time-varying gravity field model of Sichuan-Yunnan region based on the equivalent mass source model - ScienceDirect
Forced Neural Network (FNN) model
Transfers of embodied PM2.5 emissions from and to the North China region based on a multiregional input-output model - ScienceDirect
Overview of the data sets used for joint inversion. (a) Map view of the
Evidence for a developing plate boundary in the western Mediterranean
Schematic diagram of model I.
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Modelled zero offset seismic section for the start of the simulation
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Comparison of the numerical free streamline shape with the exact
The original and processed gravity responses of model III.
Histogram of generalization errors for different structures, all