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Research Collection

Educational Material

Reflection seismic 1 script

Author(s):

Kruk, Jan van der Publication Date:

2001

Permanent Link:

https://doi.org/10.3929/ethz-a-004363847

Rights / License:

In Copyright - Non-Commercial Use Permitted

This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use.

ETH Library

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Elimation of effects by

Filtering Stacking Migration

Adjust amplitudes for plotting

Improve coherency of reflections

(3)

Frequently used operations

• Time dependent frequency filter

• Coherence filter

• AGC

(4)

Reason for filtering after stacking:

• By using different filters, additional noise is generated

• Frequency content of data is changed due to different processing steps (NMO stretching)

• Time dependent frequency filter is often not

used before the stacking procedure

(5)

Aim:

Suppression of noise

Elimination of artefacts (extreme dips)

Improve amplitudes and continuity of reflections Filters:

fk-Filter

fx-deconvolution (Wiener-Levingson-Filter) Korhunen-Loeve-Filter (Eigenvector-Filter)

(6)

Amplify reflections

=> Depending on aim of interpretation:

Clear Structures

Preserve Reflection charcteristics Adapt amplitudes for Printing

Usually: AGC

(7)

Stacking / Migration

Printing on Paper Digital Storage

Safe archive Interpretation

Improved view for long profiles (e.g. SEGY-Format)

Archive

Visualisation and

Interpretation with a workstation

(8)

Data

Sidelabel

extra information:

(“Header plots”) Velocity funktion Fold

Point of intersection with other profiles Location of borehole loggings

Topography

Shotnumber (additive to CMP) etc.

(9)

Referenzen

ÄHNLICHE DOKUMENTE

This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms

This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms

This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms

This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms

This page was generated automatically upon download from the ETH Zurich Research Collection.. For more information please consult the Terms

This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms

This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms

This page was generated automatically upon download from the ETH Zurich Research Collection.. For more information please consult the Terms