1887

Abstract

Summary

The magnetic anomaly dataset was used to delineate fault parameters and terrane boundaries of the Mongolian territory. The spectral method has been implemented to separate shallow-, intermediate- and deep-seated faults and corresponding figures have been depicted. Also, locations of some new hypothetic faults have been estimated from the geomagnetic dataset.

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/content/papers/10.3997/2214-4609.201902473
2019-09-08
2024-03-29
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References

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