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Inverse Theory Definition: Inverse Theory deals with the determination of the model parameters from the data. In our case it is the estimation of subsurface structure from surface measurements. data Model Model paramete rs

Inverse Theory in Geophysics, Lecture 1

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Page 1: Inverse Theory in Geophysics, Lecture 1

Inverse TheoryDefinition:Inverse Theory deals with the determination of the model parameters from the data. In our case it is the estimation of subsurface structure from surface measurements.

data Model Model parameters

Page 2: Inverse Theory in Geophysics, Lecture 1

DefinitionA model may be defined as the mathematical relation (either analytical or empirical) that relate the independent variable X with the dependent variable Y in the form:

Y= a + b XIn this model, the model parameters are a and b. In algebraic notation they are the unknowns of the equation. In matrix form this relation may be written as:

A m = d

Page 3: Inverse Theory in Geophysics, Lecture 1

Where:

A Is the kernel or coefficients matrix

m is the vector of model parameters a & b

D is the data vector

(1 𝑥1⋮ ⋮1 𝑥𝑛

)(𝑎𝑏)=(𝑌 1

⋮𝑌 𝑛

)

Page 4: Inverse Theory in Geophysics, Lecture 1

The model here for gravity field is:

To define the theory in more practical way we use the beach example where we expect a pirates treasure is burried under the sand. The treasure is made of gold which is much more dense than sands. Thus we propose to use the gravity method.

Page 5: Inverse Theory in Geophysics, Lecture 1

The problem is that we

Thus the methodology here is forward modeling not inverse. The ideal model of the beach may be sketched as:

Page 6: Inverse Theory in Geophysics, Lecture 1

The computation algorithm we will adopt will

As we have 45 blocks we end up with:

We also end up with no unique solution.

Page 7: Inverse Theory in Geophysics, Lecture 1

The models may be categorized as:

Page 8: Inverse Theory in Geophysics, Lecture 1

Problems we face:

Why!!!Because the beach

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End of Lecture

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