Determination of Reservoir Lithology from Seismic Data by a 2D Hidden Markov Random Field Model

Conference Paper (2018)
Author(s)

Runhai Feng (TU Delft - Applied Geology)

S.M. Luthi (TU Delft - Applied Geology)

A Gisolf (ImPhys/Acoustical Wavefield Imaging )

A. W. Martinius (TU Delft - Applied Geology)

Research Group
Applied Geophysics and Petrophysics
Copyright
© 2018 R. Feng, S.M. Luthi, A. Gisolf, A.W. Martinius
DOI related publication
https://doi.org/10.3997/2214-4609.201801076
More Info
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Publication Year
2018
Language
English
Copyright
© 2018 R. Feng, S.M. Luthi, A. Gisolf, A.W. Martinius
Research Group
Applied Geophysics and Petrophysics
Bibliographical Note
Green Open Access added to TU Delft Institutional Repository ‘You share, we take care!’ – Taverne project https://www.openaccess.nl/en/you-share-we-take-care Otherwise as indicated in the copyright section: the publisher is the copyright holder of this work and the author uses the Dutch legislation to make this work public.@en
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Abstract

In this study, geological prior information is incorporated in the classification of reservoir lithologies using the Markov Random Field (MRF) technique. The prediction of hidden lithologies in seismic data is based on measured
observations such as seismic inversion results, which are associated with the latent categorical variables derived from the distribution of Gaussian assumptions. The Hidden Markov Random Field (HMRF) approach can connect
similar lithologies laterally (horizontally) while ensure a geologically reasonable stratigraphic (vertical) ordering. It is, therefore, able to exclude randomly appearing lithologies caused by errors in the inversion. In HMRF, the prior
information consists of a Gibbs distribution function and transition probability matrices. The Gibbs distribution connects similar lithologies and does not need a geological definition derived from non-case-related information.
The transition matrices provide preferential transitions between different lithologies and an estimation of these matrices implicitly depends on the depositional environments and juxtaposition rules between different lithologies.

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