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EAGE Workshop on Quantifying Uncertainty in Depth Imaging
- Conference date: April 12-13, 2021
- Location: Online
- Published: 12 April 2021
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Quantifying the Uncertainty of the Depth Where Imaging is
Authors H. BoltSummaryAlong-hole depth is the most fundamental subsurface measurement made in our business. When regarding imaging information, or any subsurface information, not knowing the along-hole depth or the uncertainty of the depth value provided renders the information of limited value. New along-hole depth measurement theory and practices and new ways of calculating uncertainty of depth measurements are presented that address the assumptions that are otherwise made. This results in quantified uncertainty rather than guessed or assumed values which can be matched to the uncertainty requirements of the data users. The matching of the methodologies used in measurement to the requirements results in an uncertainty budget that is arrived at by design rather than by assumption of guesswork.
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Quantifying Depth Uncertainty in Regional Scale – a Probabilistic Approach
Authors A.I. Yusof, L.K. Yeap and A. KhalilSummaryRegional time-to-depth conversion on frontier area is very challenging as it involves multiple seismic surveys covering thousands of square kilometre areas with very limited well control. Hence, the results would be associated with high uncertainty. This uncertainty needs to be properly quantified as it can influence basin modelling outcome, especially in terms of depth/ shape of the kitchen, charge volume and migration pathway. Our approach of regional probabilistic time-to-depth conversion which uses Bayesian co-kriging simulation ensures consistent integration of multiple sources of uncertainties throughout all layers within the probabilistic model. Hence, this method does not assume (or bias to) any base case velocity model. The output will be an estimation of depth for each individual horizon and each velocity with the associated uncertainties, providing us with not only the base case prediction but also the low and high case prediction of the full uncertainty range as derived from the simulations.
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Re-Imaging through Multi-Level, Highly Saturated Gas Bodies in a Carbonate Regime – a Case Study
Authors M. Supardy, C. Lee Slind, T. Wai Hoong, P. Ming Heng, L. Kien Kok, A. Widyanita, A. R L Desplanques, K. Xin, W. Chan, A. Azmi, S. Maitra, F. F Basir and A. Lip HunSummaryDepth imaging is almost a mandatory to wholly understand and explore a given field. Absorption effects due to shallow gas at reservoir level are common all around the world. This problem will cause un-optimum image together with the depth uncertainties if not address correctly especially at the targeted reservoir level. Tailored processing flow of Q-tomography and Q-PSDM were used to address these issues, compensating for amplitude, frequency and phase distortion in the data. The velocity plays a significant role, thus application of FWI is mandatory for this kind of environment. Pairing these velocity modelling tools with optimum de-ghosting and de-multiple improves imaging of the structure with a potential of accurate analysis underneath the shallow gas. This consequently reduced the depth uncertainties of the target reservoir.
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Minimizing Depth Error through Robust Velocity Model Building – a Case Study
Authors M.S. Sulaiman, S.F. Mohd Zohdi, C.L. Slind, P. Gabrielli and G. JamesSummaryRobust velocity model building using FWI and Tomography provides a good depth imaging solution and gives a good depth prediction at the post salt level. Below the base of salt, subject to the illumination tomography may struggle to update the model effectively hence the depth prediction at the pre-salt level may be less accurate.
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Quantifying Uncertainty in Depth Imaging : Case Histories
Authors L. SandjivySummaryAcceptance by geophysicists to discuss the reliability of the subsurface and O&G reservoir images they produce in terms of uncertainty is a major breakthrough for the industry Quantifying Uncertainty in Depth imaging is then directly linked to Quantifying Confidence in SubSurface and Reservoir models supporting multi million dollars E&P decisions. Uncertainty on seismic processing and imaging uncertainty cannot be properly quantified by geophysical processes solving inverse problems, but only by kriging algorithms specific to seismic processing, solving reservoir estimation problems. Further and deeper integration of Kriging algorithms in geophysical processing and imaging processes will certainly lead to significant optimization of the parametrization of the geophysical processes and to quantified improvement of E&P project performance
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Quantify Velocity Model Uncertainty and Its Relationship with Geobodies
Authors M.H. Pua, C. Lee Slind, I.S. Mohammad, A. Widyanita, S. Maitra and F. F BasirSummaryQuantify uncertainty had been an issue in time depth conversion and uncertainty quantification are mainly based on experience and so called gut feelings of the interpreter specifically on velocity model. There is plenty of tools in the market now allow interpreter to quantify uncertainty however it could only provide an uncertainty value based on the interpreter input of most likely uncertainty. And those software are more likely provide an uncertainty value on a surface instead of a 3D cube. With 3D cube uncertainty value, geobodies uncertainty could be also be properly quantify and form a relationship with velocity uncertainty.
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Quantifying Depth Uncertainties below Complex Overburden of Low Velocity Channels
Authors A.S. B Johari, W.L. Liew, P.A. Adriani, V. Pradhana and A. KhalilSummaryComplex overburdens of low velocity channels can obscure depth imaging due to their heterogeneous nature and lateral velocity variation. Such overburden may cause undesired effects in the form of travel-time pull-down (sag) and possible energy absorption. In depth imaging, the velocity model pertaining to such overburden is of vital importance to bring the objective level(s) to the appropriate image and the depth of reflectors. The aim of this work is to quantify the depth uncertainty using stochastic time to depth conversion method that would span the range of uncertainties of the depth maps underneath such complex overburden which shall enable full range of depth realizations to be generated, gross bulk volume (GBV) ranking that better quantifies the range of uncertainties and subsequently impacts hydrocarbon volumetric estimations.
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Quantifying Depth Imaging Uncertainty of a FWI, Q-KDM and Q-RTM Seismic Volume
Authors A. Muhamad, F. Zohdi, N. Isa, N.A. Mohamad Radzi and L. Wei LongSummaryA model building strategy was pursued to address specific imaging challenging in this survey area. Such challenges included the presence of slow shallow gas and fast carbonate layer in the overburden interval. The three main topics in this project were FWI, CIP (Common Image Point) Tomography and Q-model building. FWI and CIP tomography were used to derive a kinematically accurate velocity model while Q-model building was used to derive a geologically plausible absorption model.
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Structural Depth Uncertainties in Producing Oil Fields
Authors A. Tarang, A.M. Mawarni and A. KhalilSummaryThis paper look at the structural uncertainties in a mature producing field in Malay Basin. In general as more development wells are drilled, the structural uncertainties are becoming less, but it still exist due to - time interpretation, marker and the velocity model. Unlike in newly discovered field - associated structural uncertainties for infill well will cause drilling of expensive sidetrack. Therefore, it is equally important to investigate the role of structure uncertainties and seismic imaging which provide the image - in order to optimize further exploitation activities.
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Depth Prognosis in a Brown Field: When 6m Certainty is Inadequate
Authors S.A. Ahmad Hawari, M.A. M Diah and A.T. Patrick PantingSummaryThis paper will discuss a drilling campaign experience of a mature brown oil field in Peninsular Malaysia, where a 3 well campaign was embarked and how the team reacted to findings on-the-fly, with mixed results. We will demonstrate how the depth maps and the depth prognosis were derived, the subsequent velocity modeling uncertainty analysis carried out and the overall outcome of the drilling campaign. We will also then look into the possible root causes on the well depth results with a discussion on recommended alternative approaches for similar drilling scenarios in the future.
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Inherited Uncertainties of Advanced Depth Migrated Images
Authors R. Alai, A. Mokhtar, C.L. Slind, Y. Guo, J. Wang, P. Wardaya, R.K. Pratama and P. MonaliaSummaryThe process of optimal data preconditioning is a critical framework shaping optimum depth imaging with “accurate” locations. This process serves as input to velocity model building and its qualitative evolution for each of the processing stages. Detailed attention was undertaken to suppress unwanted energy and latest “noise-controlled” deghosting method was applied to the data, ensuring recovery of amplitude and frequency for better demultiple and imaging target zones. The total wave field was decomposed into specular reflection and diffraction data allowing their separated imaging and multi-term surface multiple estimation towards optimal velocity model estimation (FWI and tomographical velocity updates) and focused depth migrated images. Latest advanced FWI was utilized to facilitate inversions of weaker energy of lower frequencies to be modelled and updated. The final derived velocity model was cross checked and validated with measured velocities from 15+ wells with velocity mistie uncertainties below 10% due to ambiguities of the interpreted horizons. Refined horizon picking is critical for gamma analyses for depth uncertainties along the horizons. With these views, justification of each step in the process contributing to uncertainty between seismic depth images and actual geological markers from wells and most importantly away from wells is clarified and further quantified.
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A Decade of Seismic Uncertainty and the Opportunities of the Next Decade
Authors R. Bloor and D. NicholsSummaryCalculating uncertainty on seismic is a topic that has appeared a number of times over the years and inparticular we have seen more use in the last decade. We will review and examine this history and discuss the growing opportunities going forwards which we expect to be a dramatic extension of the use cases to date.
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Efficiently Measuring the Uncertainty of FWI Models and Integration with Tomography and Geology
More LessSummaryThe paper tries to analyzing the uncertainty of FWI models and the ways to mitigate through integration with tomography and geology
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A Robust Self-Supervised Learning System for Low Frequency Seismic Data Extrapolation to Reduce Model Building Uncertainty
More LessSummaryIn order to suppress the cycle-skipping phenomenon in full waveform inversion (FWI) and reduce the uncertainty resulting from velocity model building practices, we developed a Deep Neural Network (DNN) based Self-Supervised Learning method to predict the low frequency (LF) seismic data by exploiting the implicit relationship connecting the LF data and the high frequency (HF). Employing the Progressive Transfer Learning strategy that seamlessly integrates a physics-based module and a DNN module, this Self-Supervised Learning system does not require access to labelled data, which are often impractical to collect in realistic projects. Instead, the training datasets are generated and automatically labelled within the learning system. Furthermore, this Self-Supervised Learning system is able to iteratively evolve the training set and update the DNN by gradually retrieving the subsurface information through the physics-based module to enhance the LF data prediction accuracy, thus propelling the FWI process out of the local minima. Throughout the workflow, the uncertainty of the LF extrapolation is rigorously monitored and quantified by the Self-Supervised Learning system.
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Analyzing and Quantifying Uncertainty in Time-Depth Conversion
Authors J. Chautru, H. Binet, P. Masoudi, S. Rodriguez and M. PapouinSummaryStatic geological models are made of horizons and faults which define their geometry. Both faults and horizons (in depth) are uncertain objects, which result from a time-to-depth conversion procedure involving variables such as time maps, velocity maps, markers at wells that in turn might all be affected by a given level of uncertainty. Even faults location may be uncertain and impact Gross Rock Volumes (GRV) calculated in the geological model. This paper details methods which allow simultaneous calculation of depth maps and the associated uncertainty. Focus is put on how to quantify the impact on the global uncertainty on GRV of each Time-Depth conversion input parameter uncertainty. The relative impact of each individual source of uncertainty is calculated on a real case study and the quantitative effect of combining the different sources is estimated and analyzed.
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Quantifying Depth Uncertainty in Exploration to Development Cycle through Evolving Imaging Technology
Authors G. BalakrishnanSummaryBy leveraging on evolving imaging technologies, we managed to demonstrate that imaging uncertainties can be reduced, impacting efficient and safe well delivery and de-risking NFE opportunities
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Multi-azimuth Q Inverted Full Waveform Inversion: a Data-Driven Approach for Quantifying Structural Uncertainties Beneath Gas Cloud
Authors W.Y. Ham, K. Mohamed and C. LukSummaryThis abstract showcased a data driven approach i.e. Q inverted full waveform inversion that utilized dual azimuth seismic datasets. This is a method to address both the imaging and depth uncertainties on subsurface structure beneath the gas cloud. There are three elements were used for quantifying imaging and depth uncertainties such as comparison of residual move-out map, phase consistency sense check from seismic-to-well tie and total depth uncertainty maps by combining both horizon picking and velocity uncertainties maps based on the depth residual at different well locations.
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A 3D Pseudo-Spectral Method for qP-Wave Simulation in TTI Media and its Application in RTM
Authors J. Li, K. Xin, A.R.B. Ghazali and F. SyazanaSummaryA pure qP-wave equation that is free of shear-wave artefacts is usually desired during imaging seismic data in tilted transversely isotropic (TTI) media, by which, crosstalks caused by the interference between different wave modes can be eliminated. However, an undesired SVwave energy could be generated during modeling, even if an acoustic anisotropic wave equation is used. In this study, we first extend the temporal fourth-order pseudospectral time domain (PSTD) PSTD scheme to 3D qP-wavefield simulation in anisotropic media by using Zhou’s equation (Zhou et al., 2006) and the S-wave energy is still detected. And then, a new fully decoupled P-wave equation in TTI media is developed in this study to avoid unwanted energy during migration. During wavefield simulation, the finite difference (FD) and pseudospectral (PS) method are combined in order to accelerate the computation. The comparisons of phase velocities between the new decoupled wave equations and the other approximations are illustrated to validate the precision in different anisotropic medium. To eliminate the artificial boundary reflections, the H-PML in second order wavenumber domain is applied, comparisons of different absorbing boundary layers are illustrated to validate the wave number domain H-PML. The new algorithm is further applied in a new 3D anisotropic reverse time migration (RTM), which has been tested on 3D synthetic SEAM data and field data. As a result, seismic images with high resolution are produced. Benchmarks against commercial implementations are also demonstrated, which proves that the positioning of structure is more reliable and accurate with the new algorithm.
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Imaging Depth Uncertainty from an Interpreters Perspective: Implications from Processing to Assessment
Authors S. Hussenoeder, Y. You, A. Wawrzynski, D. Dykes, C. Lehmann, R. Lu and R. BloorSummaryThis presentation shows how ExxonMobil and Schlumberger are leveraging WesternGeco’s Seismic Uncertainty Analysis (SUA) technology to address seismic velocity ambiguity and associated quality & positioning of the seismic image, and provide velocity-based geometric realizations to prospect volumes assessment.
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