19 May 2012
 
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Seismic Inversion

Seismic Inversion is the process of converting seismic reflectivity data to rock property information, ranging from band-limited acoustic impedance (simplest) to petrophysical properties such as Vshale, porosity and water saturation (most complex). Rock physics is crucial in this process for a number of reasons:

  • To ensure input data (seismic and wells) are properly conditioned
  • To indicate what impedance flavours are most discriminative for the problem at hand
  • To assist in the seismic inversion algorithm itself (e.g. depth trends)
  • To assist in going from impedances to reservoir properties

 

RokDoc  provides a number of inversion QC tools, and  Seismic Conditioning Steps, to improve the results of the inversion algorithms.  Finally, impedance results are not an end in themselves; they lead to reservoir characterization, and some techniques in the RokDoc toolkit are presented

Ikon Science Seismic Inversion Algorithms

Ikon Science promote seismic inversion as a tool and not an end in itself. It can be used to good effect in reservoir characterisation from exploration to reservoir monitoring. A selection of seismic inversion algorithms exist, in house we refer to this as the seismic inversion menu. Further information on seismic inversion algorithms can be read in the Kemper paper on the subject.  This paper also explains the importance of constructing a quality Low Frequency Background Model, should an absolute impedence result be required. 

 

This seismic inversion technique introduced by Lancaster and Whitcombe in 2000 makes and applies a matching filter to map the seismic spectrum onto a more broadband 'earth spectrum' as defined from well impedance profiles. This explains the spectral blueing characteristics of this process. No wavelet is required, and the seismic inversion is band-limited, so a spectral merge with a low frequency background model may be carried out, as required.



Lancaster, S. and Whitcombe, D. [2000] Fast-track ‘coloured’ inv. 
70th SEG annual meeting, expanded abstracts 1572-1575

This essentially is spectral decomposition in the impedance domain. After a spectral decomposition into bandlets, each one is inverted to 'implets', which are then recombined to provide the spectral impedance result. No wavelet is required, and the seismic inversion is band-limited, so a spectral merge with a low frequency background model may be carried out, as required.



Figure from RokDoc

Interactive and integrated in a geological model, the stochastic inversion creates high resolution models of impedance, incorporating reservoir heterogeneities and geological trends by using geostatistical techniques honouring both well and seismic data. Consider using stochastic inversion when you want fine detail and a measure of uncertainty in that detail. Our stochastic inversion implementation is extremely interactive; many parameters can be tested and inversions can be adjusted to provide the best possible results.

Using cloud transform, a rock physics model that describes the statistical relationship between two or three impedances from log data, the stochastic inversion algorithm can be employed to provide pairswise/triplet-wise impedance realizations, so essentially an AVO stochastic inversion.

The multiple realization can be analyzed in many ways to provide the user with statistical descriptions of the reservoir, such as a PDF of volumes of hydrocarbon bearing reservoir to be expected at a to-be-drilled well location, or a P10,P50,P90 description of the NtG of a field.

Haas, A. and Dubrule, O. [1994]
Geostatical inversion - a sequential method of stochastic reservoir modeling constrained by seismic data.
First Break , 12
(11), 561-569.

Delivery is an open source www.csiro.au/products/delivery.html Bayesian Inversion program. It is considered state-of-the-art in the industry, and is virtually impossible to use as is. That's why in RokDoc we have developed a highly interactive wrapper to this tool, that exposes all its power to the user. The user has to specify all information that goes into calculating amplitudes in the form of a normal distribution, so per trace: top, base, NtG, Por, Satn, Vp, Vs, Rho etc. This information together with the seismic to be inverted is used to create a likelyhood function, from which the posterior distribution is calculated (using MCMC techniques). The posterior distribution can be analysed in any way conceivable. Delivery is the only seismic inversion tool in the market place that can invert for the position of top and base of a layer, i.e. for its thickness. Very relevant to determine in-place volumes in a flat structure: the depth of the OWC is then crucial.

Gunning, J. & Glinsky, M.E. [2004]
Delivery: an open–source model–based Bayesian seismic inversion program. Computers & Geo­sciences,
30, 619−636.

We have state of the art inversion technologies for 4D inversion, be it Neural Net or Rock Physics Model Template driven. More info in our reservoir monitoring page.

Seismic Inversion Cheat Sheet

 

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