
Seismic Coloured Inversion (now built using Qt®)
A
superior fast track method for the inversion of seismic data
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Enables the rapid
inversion of 2D/3D seismic data.
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Allows the
Interpretation Geophysicist to generate relative Acoustic Impedance in
a time frame previously thought impossible.
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Can be seamlessly
integrated with existing seismic interpretation systems and allows
Interpretation Geophysicists to gain access to inversion techniques.
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Now available as an
OpendTect plugin
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Provides a globally
optimised inversion consistent with observed behaviour from well logs.
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Rapid, robust,
inexpensive and eliminates the need for expert users.
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De-trend and
normalisation, allow the relative amplitude changes observed in the
impedance volumes to be interpreted quantitatively.
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Used in conjunction
with 4C/4D data, SCI can assist in the interpretation effort of such
data.
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Product
Description
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Inversion of seismic
data to Acoustic Impedance (AI) is usually seen as a specialist
activity. In spite of publicised benefits, inverted data are only used
in a minority of cases. To help overcome this obstacle, this new
algorithm which is quick and easy to use, can increase the use of
inversion technology. SCI performs significantly better than
traditional fast-track methods such as recursive inversion, and
benchmarks well against unconstrained sparse-spike inversion. With the
inclusion of de-trend and normalisation functionality within SCI,
geophysical meaning can now be assigned to the observed amplitude
changes in the derived impedance volumes. This can be very powerful,
particularly with 4D projects. Once the SCI operator has been derived,
it can be simply applied using the 3D processing tool included within
the SCI software. In this way, inversion can be achieved within hours
since the volume data do not have to be exported to another package.
Existing fast-track methods for band-limited inversion to relative AI
are prone to error because no account is taken of the seismic wavelet
or calibration to the Earth. Although more sophisticated techniques
such as sparse-spike inversion take account of these factors,
specialist skills are required. SCI takes into account the seismic
wavelet and is consistent with log data. With this technique, it is now
possible to routinely invert any dataset within hours and establish a
base case against which more sophisticated techniques must be judged.
SCI enables the rapid inversion of 2D/3D data. A single convolution
inversion operator is derived that optimally inverts the data and
honours available well data in a global sense. In this way, the process
is intrinsically stable and broadly consistent with known AI behaviour
in the area. Construction of the operator is a simple process and
implementation can be readily performed within the processing module
included in SCI. As an explicit wavelet is not required, other than
testing for a residual constant phase rotation as the last step, this
removes an inherently weak link that more sophisticated processes rely
on.
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Benefits
of SCI
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Generally,
traditional
inversion methods (e.g.sparse- spike) are time consuming,
expensive,require specialists and are not performed routinely by the
Interpretation Geophysicist, whereas SCI is rapid, easy to use,
inexpensive, robust and does not require expert users. SCI and
unconstrained sparse-spike appear to give broadly equivalent results.
SCI seamlessly connects with third party seismic and well data
repositories (including SeisWorks, OpenWorks and GeoFrame) using our
client/server technology. SCI is now available as an OpendTect plugin
and can be downloaded from the OpendTect downloads center. This allows
SCI analysis,operator design and
processing to be performed without separately importing or exporting
data.
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| Application Support and Maintenance |
With a support and maintenance contract from ARK
CLS Limited, clients can download software updates in the form of new
releases and patches.
Online documentation is available for SciQt standalone and for SciQt plugin |
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Qt and the Qt logo are trademarks of Trolltech in Norway,
the United States and other countries.
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