Characterizing an earth subterranean structure by iteratively performing inversion based on a function
To characterize an earth subterranean structure using a measurement assembly including electromagnetic (EM) receivers and one or more EM sources, measured voltage data collected by EM receivers in response to transmission by one or more EM sources is received. Based on a model, predicted EM data is computed. Inversion is iteratively performed according to a function that computes a difference between the measured voltage data and a product of a term containing the predicted EM data and a term containing distortion data that accounts at least for distortion effect by an environment of the measurement assembly. The inversion is iteratively performed to solve for parameters of the model and the distortion data.
1. A method of characterizing an earth subterranean structure using a measurement assembly including electromagnetic (EM) receivers and one or more EM sources, the method comprising:
receiving at a data processor measured voltage data collected by the EM receivers in response to transmission by the one or more EM sources;
generating, in the data processor, common receiver position gathers from the measured voltage data;
interpolating and resampling, in the data processor, the measured voltages to a plurality of common source positions;
computing, based on a model, predicted EM data; and
iteratively performing inversion at the data processor according to a cost function that computes a difference between the interpolated, resampled measured voltage data and a product of a term containing the predicted EM data and a term containing a correction factor for distortion caused by a near-surface man-made structural heterogeneity,
wherein iteratively performing the inversion solves for parameters of the model and the correction factor for distortion caused by the near-surface man-made structural heterogeneity.
2. A method for imaging resistivity in a formation, comprising:
receiving at a data processor measured voltage data collected by a plurality of electromagnetic (EM) receivers in a plurality of measurement positions in response to transmission by one or more EM sources;
normalizing the measured voltage data;
sorting the normalized measured voltages into one or more common receiver position gathers;
resampling and interpolating the measured voltages into a plurality of common source positions;
interpolating measured data from measurement positions the common receiver gathers and common source position data to a plurality of global positions to derive a globalized, normalized voltage data set relating to resistivity in the formation;
performing at the data processor mathematical inversion on the globalized, normalized voltage data set according to a cost function to solve for at least 1) a correction factor indicative of distortion caused by a near-surface man-made structural heterogeneity and 2) a plurality of resistivity image parameters; and
generating at a display an image of the resistivity in the formation accounting for distortion caused by a near-surface man-made structural heterogeneity.