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The start depth in gravity anomaly inversion is discussed in this paper, and a newmethod called “test comparing method” is presented to determine the start depth when both boring dataand seismic data are not available. Anticline and synline density interface models are designed to test themethed; the calculated resall agreed well with the designed value, which Proved tha the new method canbe used to determine the start depth in the guity anomal inversion when boring data and seisndc dataare not available.
The start depth in gravity anomaly inversion is discussed in this paper, and a new method called “test comparing method ” is presented to determine the start depth when both boring data and seismic data are not available. Anticline and synline density interface models are designed to test themethed; the calculated resall agreed with the designed value, which Proved tha the new method canbe used to determine the start depth in the guity anomal inversion when boring data and seisndc dataare not available.