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Journal ArticleDOI

Generalized Nonlinear Inverse Problems Solved Using the Least Squares Criterion

Albert Tarantola, +1 more
- 01 May 1982 - 
- Vol. 20, Iss: 2, pp 219-232
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TLDR
In this article, a general definition of the nonlinear least squares inverse problem is given, where the form of the theoretical relationship between data and unknowns may be general (in particular, nonlinear integrodierentia l equations).
Abstract
We attempt to give a general definition of the nonlinear least squares inverse problem. First, we examine the discrete problem (finite number of data and unknowns), setting the problem in its fully nonlinear form. Second, we examine the general case where some data and/or unknowns may be functions of a continuous variable and where the form of the theoretical relationship between data and unknowns may be general (in particular, nonlinear integrodierentia l equations). As particular cases of our nonlinear algorithm we find linear solutions well known in geophysics, like Jackson’s (1979) solution for discrete problems or Backus and Gilbert’s (1970) a solution for continuous problems.

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Citations
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Journal ArticleDOI

Low velocity crustal flow and crust-mantle coupling mechanism in Yunnan, SE Tibet, revealed by 3D S-wave velocity and azimuthal anisotropy

TL;DR: In this paper, the authors used teleseismic data recorded by a permanent seismic network in Yunnan, SE Tibet, and measured the interstation Rayleigh wave phase velocity between 10 and 60 s. A two-step inversion scheme was used to invert for the 3D S-wave velocity and azimuthal anisotropy structure.
Journal ArticleDOI

Wavelet‐based methods for the nonlinear inverse scattering problem using the extended Born approximation

Eric L. Miller, +1 more
- 01 Jan 1996 - 
TL;DR: In this article, the authors present an approach to the nonlinear inverse scattering problem using the extended Born approximation (EBA) on the basis of methods from the fields of multiscale and statistical signal processing.
Journal ArticleDOI

Inversion of needle‐probe data for sediment thermal properties of the eastern flank of the Juan de Fuca Ridge

TL;DR: In this paper, an estimation method is introduced for measuring thermal conductivity, thermal diffusivity, and heat capacity of sediment from temperatures using a needle probe. But the method is based on the continuous cylindrical heat-source model.
Journal ArticleDOI

Coupled Process Models as a Tool for Analysing Hydrothermal Systems

TL;DR: In this article, numerical simulations of hydrothermal processes can be used to better understand coupled reactive transport in modern geothermal systems and in ancient geothermal ore deposits, based on the Enhanced Geothermal System at Soultz-sous-Forets in France, and the geothermal resource at Hamburg-Allermohe in Germany.
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A Gaussian-based framework for local Bayesian inversion of geophysical data to rock properties

TL;DR: A procedure for inverting rock properties based on geophysical data in which few and weak assumptions are required for application to various inverse problems within the geophysical industry is derived.
References
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Book

Linear statistical inference and its applications

TL;DR: Algebra of Vectors and Matrices, Probability Theory, Tools and Techniques, and Continuous Probability Models.
Journal ArticleDOI

Uniqueness in the Inversion of Inaccurate Gross Earth Data

TL;DR: In this article, it was shown that a given set G of measured gross Earth data permits such a construction of localized averages, and if so, how to find the shortest length scale over which G gives a local average structure at a particular depth if the variance of the error in computing that local average from G is to be less than a specified amount.
Journal ArticleDOI

The general linear inverse problem - Implication of surface waves and free oscillations for earth structure.

TL;DR: In this paper, the discrete general linear inverse problem is reduced to a set of m equations in n unknowns and a linear combination of the eigenvectors of the coefficient matrix can be used to determine parameter resolution and information distribution among the observations.