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EAGE/SEG Workshop - Depth Imaging of Reservoir Attributes
- Conference date: 02 Aug 1998 - 04 Aug 1998
- Location: Boussens, France
- ISBN: 978-94-6282-122-4
- Published: 02 August 1998
21 - 38 of 38 results
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AVO Principles of Time and Depth Processing - Part 2 - Applications
Authors W. Beydoun and C. HanitzschThe text of this abstract is included in abstract: AVO Principles of Time and Depth Processing - Part 1 - Basic Principles
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Some Aspects of AVO Inversion in Depth
Authors A. Canning, A. Malkin and S. GibliAbstract was made available at the workshop
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True Amplitude Prestack Imaging of Converted Waves
Authors L. Nicoletis, J. Svay-Lucas and H. PrigentThe interest for P-S waves processing and interpretation has been recently enhanced by the acquisition of OBC data. As a matter of fact, S-waves recorded on the sea bottom present generally a good signal-to-noise ratio and appear promising for reservoir description.
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3D Ray + Born or Ray + Kirchoff Migration/Inversion - State of the Art
Authors P. Thierry and J. Pajchel3-D ray + Born and 3-D ray + Kirchhoff migration/inversion schemes are considered as the most accurate tools for quantitative depth imaging in 3-D heterogeneous media. The both formulations are presented here with a brief theoretical review and some comparisons on a 3-D real data set. Important theoretical and practical points (such as acquisition footprints, velocity model quality, image post-processing) are underlined with the help of Common Offset gathers in order to anderstand the method capacities for subsequent reservoir attribute studies.
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Ray + Born Migration/Inversion in Complex Media - Application to Marmousi
Authors S. Operto, S. Xu and G. LambaréWe show with an application to the complex Marmousi model, that ray + Born migration/inversion recovers quantitatively the amplitude of the impedance perturbations even in case of heavily triplicated ray fields.
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Maslov + Born Migration/Inversion in Complex Media
Authors S. Xu and G. LambaréThe limitations of classical ray theory, in case of triplicated ray fields, are well known singularities at caustics, shadow zones, ... Lots of theoretical works have been done for avoiding these artefacts.
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Imaging Beneath Gas Affected Sediments
More LessEkofisk Field exhibits a classic case of gas in the overborden destroying the image obtained from surface seismic by delaying and distorting the propagation of wavefronts. This is a very long standing problem: the field was developed with rigs set up on the northern and southern ritus, around the apparently collapsed centre. The first production well drilled into the middle came in fifteen hundred feet high to prognosis, showing the full site of the field and the effects of the gas. 30 years later about 60% of the crestal area bas been successfully imaged by undershooting the gas with 3D borehole profiles. The complete image, however, will be obtained only when a more complete onderstanding of the velocity structure of the gas has been achieved.
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A Comparison of Prestack Reservoir Attributes Using Different 3D Prestack Migration Methods
Authors J. Young, J. Krebs and C. J. FinnEven when subsurface velocities vary only moderately, accurate imaging of reservoir attributes in depth remains a challenge. Two crucial components of the solution are the determination of an accurate velocity model and the use of an appropriate imaging algorithm. We examine the depth accuracy and qualitative AVO response of images generated using different velocity models and different imaging methods. We conclude that velocities determined from offset checkshot data in conjunction with a 3-D Kirchhoff imaging algorithm yield prestack images whose depths and amplitudes are in better agreement with well data than 3-D prestack migration implemented as a multi-step process (MZO cascaded with zero offset migration).
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Utilisation of Sub-Salt Attributes from 3D Prestack Depth Migrated Seismic Data - Examples from the Greater Mickey Area, Deepwater Gulf of Mexico
Authors E. Ekstrand, T. Summers, S. Lopez-Mora and S. DavisThe majority of sub-salt seismic data throughout the Gulf of Mexico is characterised by poor signal to noise ratios degending on the complexities of structure and salt geometry. Therefore interpretation of sub-salt prospects is primarily done through structural mapping and qualitative use of attributes. An increase in demand for quantitative use of sub-salt attributes is expected as the industry continues to explore, appraise and develop future sub-salt discoveries (in the Gulf of Mexico and worldwide).
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Velocity as an Attribute - Continious Velocity Estimation from PreSDM CRP Gathers
Authors I. F. Jones, H. Baud and A. StrachanHere we present a technique for estimating the velocity associated with a final preSDM image in great detail. Essentially we employ techniques of continuons velocity estimation used for iterative model update, but apply them in a different context. Rather that using the velocity estimator strictly for velocity model building (on a set of sparse lines), we employ the estimation techniques to the ARP gathers resulting from the final migration for all CRPs in the 3D survey. This achieves two things: firstly it estimates a residual velocity correction for stacking the final CRP gathers to obtain an enhanced image, and secondly, it delivers a dense estimate of velocity for the entire 3D volume in a geologically coherent manner. It is this second feature which is the subject of this paper.
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Seismic Attribute Analysis of 3D Prestack Migration
Authors W. E. A. Rietveld, K. J. Marfurt and J. H. KommedalIn recent years, 3-D prestack depth migration bas become a common tool to image complex geology, allowing us to correctly position steeply dipping reflectors and collapse diffraction hyperbolae at reflector/fault plane terminations. In addition to collapsing major diffractions associated with accurate structural imaging, 3-D prestack migration also collapses smaller diffraction hyperbalae associated with on-lap, off-lap, clinoforms and angular unconformities necessary to accurately map stratigraphic sequences, even in the absence of complex structure
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Acoustic Impedance Estimation and Tomographic Imaging in the Vienna Basin
Authors A. Vesnaver, G. Böhm, G. Madrussani, G. Rossi and H. GranserIn the Vienna Basin are located important hydrocarbon reservoirs, characterised by fractured rocks in a complex fault system. The pre-stack depth migration is a basic tool for identifying the major geological formations. This method is particularly effective when the necessary macro-model for the velocity field and layer interfaces is provided by seismic tomography. There is a trade-off, However, from the practical point of view: seismic tomography is more necessary for relevant complexities but, in such cases, the picking of traveltimes becomes extremely difficult, if not unfeasible. So a goal of our work was to verify the effectiveness of the tomographic imaging in this difficult area.
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Imaging at Emblar Field
Authors J. A. Dangerfield, H. Raymondi, O. Fjeld and P. HaskeyIn any field development project the starting requirements are a good image, good well ties and reliable depth conversion. The Embla field represents an extreme example of the problems of seismic imaging beneath an overborden with strong lateral velocity variations, with poor matches to well synthetic seismograms, and major uncertainties in true depth prediction.
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Rational Geophysical Strategy of Reservoirs Delineation and Monitoring
Authors V. G. Budanov, A. B. Beklemischev, O. A. Potapov, B. S. Lokshin and T. V. PeshayaWe present the new data of the delineation of reservoirs and connected fault zones based on the simultaneous registration of the readings of a specially selected group of high precision gravimeters and measurement of natural microseisms.
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Reservoir Oil-Gas Bearing in Mesozoic Foundation of Kura Depression (Deconsolidation Rock)
By G. BayramovaIn 1971-1975, a field, entirely new to azerbaijan, was discovered in the Middle Kura basin. It is the Muradkhanly field . The bulk of its oil reserves was concentrated in the vilcanogenic reservoir rocks (3.000 in down) as well as the over lapping Miocene and Eocene sedimentary deposits. A similar volcanogenic reservoir rocks was stripped by the Saatly bore hole at depths ranging from 3 .540 m to 4.060 m.
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Removing Acquisition Footprint on 3D Ray-Born Inversion of the Overthrust Model
Authors S. Operto, G. Lambaré, P. Podvin and P. ThierryOperto et al. (1997) presented an application of 3D ray+Born inversion to an onshore-type sub-dataset for imaging a dip section of the SEG/EAGE Overthrust model.
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Impact of Geometry of Minimum Data Sets on 3D Velocity Analysis
By N. BienatiThe principle underlying migration velocity analysis techniques is that pre-stack migration of different data sets through an incorrect velocity model yields different reflector images, one for each data set. This means that the improvement of velocity model can be guided by the minimisation of depth differences between these images.
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Coherent AVO Picking
Authors S. Grion, A. Mazotti and U. SpagnoliniAn erroneous amplitude picking can severely degrade AVO (Amplitude Versus Offset) analysis results and may lead to incorrect drilling decisions. A major cause of errors in AVO picking is the presence of coherent and incoherent noise that interfere with the target reflection. AVO picking is therefore a crucial step in AVO analysis and care must be taken in the rejection of coherent noise and in the exploitation of the available range of incidente angles. The joint estimation of AVO and kinematic parameters (JAK: Joint Amplitude and Kinematic) (Grion, Mazzotti, Spagnolini, 1998) is an AVO picking technique that meets these requirements.
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