CONSISTENCY REGIONS IN NON-LINEAR INVERSION

dc.contributor.authorKennett B.L.N.
dc.date.accessioned2022-09-22T08:19:14Z
dc.date.available2022-09-22T08:19:14Z
dc.date.issued2004
dc.description.abstractA disadvantage of fully non-linear methods of inversion, through exploitation of the properties of model space, is the absence of a well-developed framework for error assessment. To rectify this problem an auxiliary weighting function for ensemble properties is introduced that can be used with suitable thresholds to define consistency regions of suitable models. This approach requires neither a detailed knowledge of the misfit distribution nor an underlying probabilistic model. The use of a polyhedral representation of such consistency regions is illustrated with an example from non-linear seismic event location, showing the effect of different choices for the misfit measure.
dc.description.abstractThe auxiliary weight function can be used directly with the composite misfit measure used to drive the exploration of model space in the non-linear inversion. Such composite measures usually combine a data misfit and regularization term. However, considerable benefit can be obtained by storing the data misfit and associated model characteristics for each investigated model, as well as the composite measure. The properties of the model ensemble can then be used retrospectively to define preferred models by the intersection of a consistency region in data misfit with zones constrained by desirable model properties.
dc.identifierhttps://elibrary.ru/item.asp?id=6524319
dc.identifier.citationGeophysical Journal International, 2004, 157, 2, 583-588
dc.identifier.issn0956-540X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/38695
dc.subjectEVENT LOCATION
dc.subjectMODEL UNCERTAINTY
dc.subjectNONLINEAR INVERSION
dc.titleCONSISTENCY REGIONS IN NON-LINEAR INVERSION
dc.typeСтатья

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