Depth-varying-to-density earth crust extension coefficient thermal calibration gravity anomaly retrieval method
A depth-variable density and gravity anomaly technology, applied in seismic signal processing and other directions, can solve problems such as crustal density changes and gravity interpretation distortion
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[0060] refer to figure 1 , the depth-variable-density crustal extension coefficient thermally corrected gravity anomaly inversion method of this embodiment includes the following steps:
[0061] a. Calculation of lithospheric thermogravity anomalies
[0062] According to the collected ocean magnetic anomaly data, the magnetic stripes are identified, and the ocean age isochrone is inferred, or the lithospheric thermal equilibrium time t can be obtained by referring to the existing ocean age isochrone data:
[0063] According to the measured seabed heat flow data, calculate the model thermal disturbance temperature T z :
[0064] T z = 2 T m π Σ n = 1 ∞ ( - 1 ...
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