SEG Technical Program Expanded Abstracts 2007 2007
DOI: 10.1190/1.2792781
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Quantitative stratigraphic inversion: Numerical study

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“…Specifically, the original NA was modified to seek multiple models within the calibration constraints and with input parameters that are as different as possible, in order to obtain samples from all the different combinations of uncertain parameters that can yield valid models. The modifications include (1) the use of error thresholds for the identification of calibrated models found during the inversion process ( Figure 5A, 5B), and (2) the ability to shift the search to new areas of the parameter space once low-error-model regions have been oversampled (i.e., local minima, Figure 5A; Sambridge and Mosegaard, 2002;Sharma, 2006). The inversion algorithm is run for several iterations until a stopping criterion (such as a predefined number of iterations or number of calibrated models found) is met ( Figure 5C).…”
Section: Accommodationmentioning
confidence: 99%
“…Specifically, the original NA was modified to seek multiple models within the calibration constraints and with input parameters that are as different as possible, in order to obtain samples from all the different combinations of uncertain parameters that can yield valid models. The modifications include (1) the use of error thresholds for the identification of calibrated models found during the inversion process ( Figure 5A, 5B), and (2) the ability to shift the search to new areas of the parameter space once low-error-model regions have been oversampled (i.e., local minima, Figure 5A; Sambridge and Mosegaard, 2002;Sharma, 2006). The inversion algorithm is run for several iterations until a stopping criterion (such as a predefined number of iterations or number of calibrated models found) is met ( Figure 5C).…”
Section: Accommodationmentioning
confidence: 99%