IPTC Title: High Resolution, Simultaneous VSP and Land Seismic Acquisition. Scott Robinson, Qatar Petroleum
|
|
- Valentine Anderson
- 6 years ago
- Views:
Transcription
1 Title: High Resolution, Simultaneous VSP and Land Seismic Acquisition Authors Scott Robinson, Qatar Petroleum primary author o P. O. Box 47, Doha, Qatar; (+974) ; s_robinson@qp.com.qa Salva R Seeni, Qatar Petroleum o P. O. Box 47, Doha, Qatar; (+974) ; seeni@qp.com.qa Michel Denis, CGGVeritas o 1, Rue Leon Migaux, 9134 Massy Cedex, France; (+33) ; michel.denis@cggveritas.com Saleh Barakat, VSFusion o P. O. Box 15425, Manama, Kingdom of Bahrain; (+973) ; saleh.barakat@vsfusion.com This is appropriate to be included in the following sessions: #32: New Advances in Geophysics or #39: Quantitative Geophysics: Data Acquisition to Reservoir Model Abstract The Dukhan field is a large oil field in Qatar established in 1941; it contains over 700 wells producing from 4 major reservoirs. There has been a complex history of production & development strategies used at Dukhan; starting with natural pressure depletion for more than 20 years, followed by power water injection since 1989 and gas cap cycling since Over its lifespan the Dukhan field has witnessed large changes in technology and its application. In order to maximize the long term economic recovery from the field, QP is committed to applying leading edge technologies as appropriate to aid in field development. New, state of the art, 3D seismic data combined with updated reservoir models will enable QP to continue to develop Dukhan field for many years in the future. This paper presents a case study relating to the 3D high resolution seismic acquisition currently in progress over the Dukhan Field in Qatar. Presented is how 3D VSP and surface seismic are being simultaneously acquired so as to use the VSP data to enhance the surface seismic project in: processing, interpretation and reservoir characterization. The combination of numerous 18 August, 2009 Page 1
2 VSP s and extremely high resolution seismic is unique to the industry, and offers an excellent example of how the next generation of seismic data are being acquired and used to give much higher resolution, quantitative interpretations. Design The tool used for the 3D VSP operations is a telemetric 100 levels tool with 3 components in each tool. Coupling is achieved through an articulated arm powered through the cable. The choice of the VSP tool helped to design an acquisition able to fulfill several key imaging tasks. The 100 levels tools with 15m between tools delivered a total logged depth of 1485m inside the borehole. Figure 1: Tool anchoring device Figure 2 : Tool electronic device The design should deliver the following information: - High resolution data from reservoir level (Arab D) up to the Mauddud formation, requiring a very long cable from reservoir at 2100m until 900m depth for Mauddud. - Fracture and anisotropy study at Arab D level requiring 180m of cable below the base of Arab D. - Have an optimized vertical seismic calibration over the whole depth to refine seismic surface processing. The inter bed multiples (or seismic events of similar effects) are one of the issues encountered by the processing of the previous pilot data in D modeling was preformed over dip and strike directions with a model including all the main geological interfaces in depth with their interval velocities. Sources were offset as far as 2.5km from the borehole and coverage maps were compared with different maximum offset for source points. Synthetic response for direct and reflected PP and PS waves were studied for different offsets in order to evaluate the differential between PP and PS waves for an optimum wavefield separation. Finally the effect of recording the full set of sources per swath in the East West dip 18 August, 2009 Page 2
3 direction was also studied, as it was cost effective, the swath acquisition progress being North South. In this case maximum offset in the dip direction were reaching 3.5km. In conclusion the source polygon to be acquired around the borehole was a rectangle area including the full swath length in the East West direction along 4km in the strike (North South) direction. The 100 level tool should have its deepest tool 180m below the Arab D reservoir level and consequently the shallowest one should be inside the Mauddud formation. In any case the minimum offset threshold was set at 1250m meaning that all the source points inside this radius should be acquired W E Simsima Lafan Mauddud Coverage Yamama Arab - D Khuff Figure 3: Modeling by ray tracing in the East West direction Acquisition As all the source points belonging to each 3D VSP were also seismic points of the surface seismic it was set from the start that the surface will never wait or be put on stand-by during the VSP operations. The challenges were quite important: - Rig up the 100 level VSP tool in time, demonstrate the perfect state of the equipment and record a rig source on the whole depth of the borehole before the surface seismic reach the source patch common with the VSP. The sweep used for the zero offset VSP had a much higher frequency bandwidth than the production one (200 Hz high instead of 120 Hz), in order to have a high frequency VSP log to help calibration with the surface seismic and wire-line logs. - Record several tens of thousand of source points with the tool inside the borehole without any major breakdown, and this for an average acquisition time of 10 days. The threshold for a major breakdown was set at two consecutive levels down out of August, 2009 Page 3
4 - The surface acquisition is done with the technique, which is a simultaneous type of recording where four source points are acquired simultaneously. The synchronization between the surface set up and the borehole recording systems for the sources needed to be implemented during a very short time frame just after the full borehole tool set up is operational inside the hole. - For QC purpose, the VSP data will be correlated real time to evaluate the quality and perform some simple processing tasks such as rotation of the horizontal component s. The final data set need to have the same separation algorithm than the surface seismic applied in order to recover the individual source points. This will be done on site before shipment for VSP processing. The first 3D VSP was acquired late June 2009, the second one mid July 2009 and the third one late August For the first VSP, only 75 levels were operating but synchronization and separation were successfully implemented. On the second 3D VSP over source points were simultaneously recorded both in the surface and borehole recorder in about 10 days without any breakdown of the 100 levels inside the well. A deployment system was used for the second operations in order to secure the 100 connections during the rig-up phase. A fast evaluation of the data demonstrated an excellent quality data set inside a fully cased borehole and a excellent vector fidelity of the borehole tool. Figure 4: Borehole tool testing in deployment Figure 5: Borehole deployments racks 18 August, 2009 Page 4
5 PP down PP up PP up PS down PS up SS down Figure 6: Source point offset 1500m component Z, Y, Y, HR, HT, R & RT Interpretation of former VSP data A certain number of former zero offset VSP were evaluated and reprocessed on a reduced scale in order to understand some particular physical properties of seismic rays in the Dukhan field. For DKG28 VSP which is quite interesting as it reaches the Khuff formation there is a clear indication on the P direct arrival of a diffraction caused by an accident at Top Kharaib level followed at depth by a secondary arrival event refracted along the accident. This is correlated by surface seismic interpretation. 18 August, 2009 Page 5
6 trace 6 = 439, 07ft/kb T77 Arab-D trace 248 = ft/kb Signature = L 500 ms Refor 1.7 Gain 30 Diffracted event generated by an accident around Top-Kharaib level-3450ft (?), followed at depth by a secondary arrival event refracted along the accident, with apparent velocity slightly higher than direct arrival. Figure 7: Refracted event generated by an accident at Kharaib level on DKG28 zero offset VSP W- E- Accident possibly seen by the DKG28 VSP, from 650ms extending down to Arab-D Structure map at Mauddud Figure 8: Extension of accident seen on VSP, on former surface seismic on left and on Mauddud structural map 18 August, 2009 Page 6
7 Processing The processing sequence to process the 3D Cube in P mode is quite standard with the following steps: - 3C data QC, analysis and editing. - Geometry QC and update - 3C first arrival time picking - 3 Components rotations - Wavefield separation - Spherical divergence gain correction - Deconvolution - Shot statics - Velocity model building - Vector Kirchhkoff migration - Integration with surface seismic data One good QC of a proper geometry update and overall direct arrival quality is the first arrival pick time seen as an attribute. Results Technical Contribution The first point to make on technical contribution is that several very complete seismic VSP records were successfully acquired simultaneously with a major 3D surface seismic program. By using 100 receiver nodes there was no need to shift the VSP receivers to record the desired interval, therein eliminating the need to repeat 1000 s of shots specifically for VSP acquisition. Processing seismic data acquired over carbonate strata has unique problems associated with the relatively high rock velocities and the nature of carbonate and evaporate strata to generate inter bed multiples or reflections which contaminate the seismic record. Much of the processing sequence is based on algorithms that reduce or eliminate inter bed multiples; with the 18 August, 2009 Page 7
8 simultaneous acquisition of 3D VSP s we were much better able to identify where multiples contaminated the surface seismic data allowing parameters in the attenuation algorithms to be tuned to the most aggressive level without compromising the true signal. Finally this paper presents an exceptional case for combining a variety of data acquisition objectives to meet the demands of modern reservoir characterization project. Establishing high expectations pushed industry limits leading to a premium dataset that is clearly able to extract petrophysical properties at 2 to 4 times thinner increments than was possible from previous data. 18 August, 2009 Page 8
Maximizing the value of the existing seismic data in Awali field Bahrain, by utilizing advanced 3D processing technology.
Maximizing the value of the existing seismic data in Awali field Bahrain, by utilizing advanced 3D processing technology. Eduard Maili* (OXY - Tatweer), Scott Burns (OXY), Neil Jones (Consultant, OXY)
More informationZero offset VSP processing for coal reflections
Zero offset VSP processing for coal reflections Salman K. Bubshait and Don C. Lawton ABSTRACT Shlumberger has acquired five VSP surveys on behalf of EnCana in Alberta. The primary goal of the VSP surveys
More informationADVANTAGES AND DISADVANTAGES OF SURFACE AND DOWNHOLE SEISMIC ILLUSTRATED BY PROCESSING RESULTS OF 3D VSP AND 3D+VSP
P3 ADVANTAGES AND DISADVANTAGES OF SURFACE AND DOWNHOLE SEISMIC ILLUSTRATED BY PROCESSING RESULTS OF 3D VSP AND 3D+VSP A.A. Tabakov* & K.V. Baranov** (* CGE JSC, Moscow, ** GEOVERS Ltd., Moscow) Abstract.
More informationP312 Advantages and Disadvantages of Surface and Downhole Seismic Illustrated by Processing Results of 3D VSP and 3D+VSP
P312 Advantages and Disadvantages of Surface and Downhole Seismic Illustrated by Processing Results of 3D VSP and 3D+VSP A.A. Tabakov* (Central Geophysical Expedition (CGE) JSC) & K.V. Baranov (Geovers
More informationTu A11 01 Seismic Re-processing and Q-FWI Model Building to Optimise AVO and Resolution in the Shallow Wisting Discovery
Tu A11 01 Seismic Re-processing and Q-FWI Model Building to Optimise AVO and Resolution in the Shallow Wisting Discovery G. Apeland* (WesternGeco), P. Smith (WesternGeco), O. Lewis (WesternGeco), S. Way
More informationW015 Full-waveform Seismic Inversion at Reservoir Depths
W015 Full-waveform Seismic Inversion at Reservoir Depths T. Nangoo* (Imperial College London), M. Warner (Imperial College London), J. Morgan (Imperial College London), A. Umpleby (Imperial College London),
More informationPrinciples and Techniques of VSP Data Processing
Principles and Techniques of VSP Data Processing A.A. TABAKOV, V.N. FERENTSI Geovers Ltd., Narodnogo Opolcheniya St., 38/3, Moscow, Russia. H.GARVINI Geofields Ltd., Av.13 # 8060 OFICINA 301, Bogota, Colombia
More information4D Seismic Inversion on Continuous Land Seismic Reservoir Monitoring of Thermal EOR
4D Seismic Inversion on Continuous Land Seismic Reservoir Monitoring of Thermal EOR Laurene Michou, CGGVeritas, Massy, France, laurene.michou@cggveritas.com Thierry Coleou, CGGVeritas, Massy, France, thierry.coleou@cggveritas.com
More informationCoupled Wave Field Migration. Coupled Wave Field Migration
Coupled Wave Field Migration Coupled Wave Field Migration Vp=1650 m/s T=750 ms Vp=4000 m/s Surface seismic exploration uses reflected and refracted waves for imaging purposes. In this case, special conditions
More informationFracture Quality from Integrating Time-Lapse VSP and Microseismic Data
Fracture Quality from Integrating Time-Lapse VSP and Microseismic Data Mark E. Willis, Daniel R. Burns, Rongrong Lu, M. Nafi Toksöz, Earth Resources Laboratory Dept. of Earth, Atmospheric, and Planetary
More informationP068 Case Study 4D Processing OBC versus Streamer Example of OFON filed, Block OML102, Nigeria
P068 Case Study 4D Processing OBC versus Streamer Example of OFON filed, Block OML102, Nigeria T. Castex* (Total SA), P. Charrier (CGG), M.N. Dufrene (Total SA) & C. Orji (EPNL) SUMMARY This case study
More informationMain Menu. Summary. Survey Design
3D VSP acquisition and 3C processing on a deep subsalt prospect in the Gulf of Mexico John Graves, Steve Checkles, Jacques Leveille, Hess Corporation, Houston; Allan Campbell*, Scott Leaney, C. Peter Deri,
More informationIPTC PP. Survey Planning
IPTC-13616-PP Dukhan 3D: An Ultra High Density, Full Wide Azimuth Seismic Survey for the Future Salva R Seeni, Qatar Petroleum; Scott Robinson, Qatar Petroleum; Michel Denis, CGGVeritas; Patrick Sauzedde,
More informationGeogiga Seismic Pro 9.0 Release Notes
Geogiga Seismic Pro 9.0 Release Notes Copyright 2018, All rights reserved. Table of Contents Introduction...1 Part 1 New Modules...3 Modeling2D...3 Surface RT...4 Part 2 General Enhancements...5 Part 3
More informationMitigating Uncertainties in Towed Streamer Acquisition and Imaging by Survey Planning
Mitigating Uncertainties in Towed Streamer Acquisition and Imaging by Survey Planning M.T. Widmaier* (Petroleum Geo-Services) SUMMARY Uncertainties in seismic images or reservoir characterisation can very
More informationY015 Complementary Data-driven Methods for Interbed Demultiple of Land Data
Y015 Complementary Data-driven Methods for Interbed Demultiple of Land Data S. Sonika* (WesternGeco), A. Zarkhidze (WesternGeco), J. Heim (WesternGeco) & B. Dragoset (WesternGeco) SUMMARY Interbed multiples
More informationCommon Reflection Angle Migration (CRAM) for improved input to reservoir description an example from Mumbai High Field
P-313 Summary Common Reflection Angle Migration (CRAM) for improved input to reservoir description D.P. Sinha, Apurba Saha, A. Ghosh, ONGC; Dean K. Clark*, Paradigm A new seismic subsurface imaging technology
More informationcv R z design. In this paper, we discuss three of these new methods developed in the last five years.
Nick Moldoveanu, Robin Fletcher, Anthony Lichnewsky, Darrell Coles, WesternGeco Hugues Djikpesse, Schlumberger Doll Research Summary In recent years new methods and tools were developed in seismic survey
More informationC009 Wide Azimuth 3D 4C OBC A Key Breakthrough to Lead to the Development of Hild Field
C009 Wide Azimuth 3D 4C OBC A Key Breakthrough to Lead to the Development of Hild Field D. Vaxelaire* (Total SA), K. Kravik (Total E&P Norge), F. Bertini (Total E&P Norge) & J.M. Mougenot (Total SA) SUMMARY
More informationEffect of Structure on Wide Azimuth Acquisition and Processing
P - 71 Effect of Structure on Wide Azimuth Acquisition and Processing Bruce VerWest and Dechun Lin, CGGVeritas, Houston, TX Summary This model study shows that narrow azimuth acquisition may be adequate
More informationA Short Narrative on the Scope of Work Involved in Data Conditioning and Seismic Reservoir Characterization
A Short Narrative on the Scope of Work Involved in Data Conditioning and Seismic Reservoir Characterization March 18, 1999 M. Turhan (Tury) Taner, Ph.D. Chief Geophysicist Rock Solid Images 2600 South
More informationM. Warner* (S-Cube), T. Nangoo (S-Cube), A. Umpleby (S-Cube), N. Shah (S-Cube), G. Yao (S-Cube)
Tu A12 15 High-Resolution Reflection FWI M. Warner* (S-Cube), T. Nangoo (S-Cube), A. Umpleby (S-Cube), N. Shah (S-Cube), G. Yao (S-Cube) Summary We demonstrate reflection FWI on a less-than-ideal 3D narrow-azimuth
More informationGeogiga Seismic Pro 8.0 Release Notes
Geogiga Seismic Pro 8.0 Release Notes Copyright 2015, All rights reserved. Table of Contents Introduction...1 Part 1 General Enhancements...3 Trace Display...4 Color Section Display...6 Curve Plotting...8
More informationDUG HAS EXTENSIVE EXPERIENCE WITH COMPLEX DEPTH IMAGING PROJECTS FROM ALL MAJOR OIL AND GAS PRECINCTS
DEPTH IMAGING DUG HAS EXTENSIVE EXPERIENCE WITH COMPLEX DEPTH IMAGING PROJECTS FROM ALL MAJOR OIL AND GAS PRECINCTS This combined experience, along with our advanced toolkit, means that we are ready and
More informationDELINEATION OF TIGHT GAS SANDS BY 3D-3C VSP
DELINEATION OF TIGHT GAS SANDS BY 3D-3C VSP Yousheng Yan1, Zengkui Xu1, Mingli Yi1, Xin Wei1 1. BGP, China National Petroleum Corporation Keywords: 1.delineation, 2.3D-3C VSP, 3.multi-component, 4.tight
More information3-D vertical cable processing using EOM
Carlos Rodriguez-Suarez, John C. Bancroft, Yong Xu and Robert R. Stewart ABSTRACT Three-dimensional seismic data using vertical cables was modeled and processed using equivalent offset migration (EOM),
More informationu = v is the Laplacian and represents the sum of the second order derivatives of the wavefield spatially.
Seismic Elastic Modelling Satinder Chopra, Arcis Corporation, Calgary, Canada Summary Seismic modeling experiments were performed to understand the seismic responses associated with a variety of subsurface
More informationWave Imaging Technology Inc.
Applications of wave imaging technologies to improve onshore US prospecting Morgan Brown Pacific Coast Section SEG Luncheon September 22, 2010 Wave Imaging Technology Inc. Talk Summary (45 min) WIT: Wave
More informationG034 Improvements in 4D Seismic Processing - Foinaven 4 Years On
G034 Improvements in 4D Seismic Processing - Foinaven 4 Years On C. Lacombe* (CGGVeritas UK), S. Campbell (BP Aberdeen) & S. White (CGGVeritas UK) SUMMARY Using a case history from West of Shetlands, the
More informationA Geomodeling workflow used to model a complex carbonate reservoir with limited well control : modeling facies zones like fluid zones.
A Geomodeling workflow used to model a complex carbonate reservoir with limited well control : modeling facies zones like fluid zones. Thomas Jerome (RPS), Ke Lovan (WesternZagros) and Suzanne Gentile
More informationSummary. Introduction
Chris Davison*, Andrew Ratcliffe, Sergio Grion (CGGeritas), Rodney Johnston, Carlos Duque, Jeremy Neep, Musa Maharramov (BP). Summary Azimuthal velocity models for HTI (Horizontal Transverse Isotropy)
More informationUsing Primaries and Multiples to Extend Reservoir Illumination for Time-lapse Monitoring - Application to Jubarte PRM
Using Primaries and Multiples to Extend Reservoir Illumination for Time-lapse Monitoring - Application to Jubarte PRM D. Lecerf* (PGS), A. Valenciano (PGS), N. Chemingui (PGS), S. Lu (PGS) & E. Hodges
More informationDesign of Surface Seismic Programs for CO2 Storage Monitoring. WesternGeco North America Geophysics Manager Houston
Design of Surface Seismic Programs for CO2 Storage Monitoring Mark S. Egan WesternGeco North America Geophysics Manager Houston Objectives Baseline seismic program Structure & stratigraphy of the storage
More informationWe Survey Design and Modeling Framework for Towed Multimeasurement Seismic Streamer Data
We-04-12 Survey Design and Modeling Framework for Towed Multimeasurement Seismic Streamer Data K. Eggenberger* (Schlumberger), P. Christie (Schlumberger), M. Vassallo (Schlumberger) & D.J. van Manen (Schlumberger)
More informationMitigation of the 3D Cross-line Acquisition Footprint Using Separated Wavefield Imaging of Dual-sensor Streamer Seismic
Mitigation of the 3D Cross-line Acquisition Footprint Using Separated Wavefield Imaging of Dual-sensor Streamer Seismic A.S. Long* (PGS), S. Lu (PGS), D. Whitmore (PGS), H. LeGleut (PGS), R. Jones (Lundin
More informationBorehole Seismic Services Data processing, imaging and dedicated expertise
Borehole Seismic Services Data processing, imaging and dedicated expertise To reduce risk and optimize recovery, you need a clear picture of the reservoir. OptaSense Borehole Seismic Services help you
More informationMulticomponent wide-azimuth seismic data for defining fractured reservoirs
Multicomponent wide-azimuth seismic data for defining fractured reservoirs Evaluating and exploiting azimuthal anisotropy Data Processing Figure 1 A typical surface outcrop showing aligned fractures Figure
More informationMethodology of VSP data processing
Methodology of VSP data processing A.A. TABAKOV, V.N. FERENTSI Geovers Ltd., Narodnogo Opolcheniya St., 38/3, Moscow, Russia. ABSTRACT Vertical seismic profiling is a powerful and widely implemented method
More informationAVO Analysis with Multi-Offset VSP Data
AVO Analysis with Multi-Offset VSP Data Z. Li*, W. Qian, B. Milkereit and E. Adam University of Toronto, Dept. of Physics, Toronto, ON, M5S 2J8 zli@physics.utoronto.ca T. Bohlen Kiel University, Geosciences,
More informationEarthStudy 360. Full-Azimuth Angle Domain Imaging and Analysis
EarthStudy 360 Full-Azimuth Angle Domain Imaging and Analysis 1 EarthStudy 360 A New World of Information for Geoscientists Expanding the Frontiers of Subsurface Exploration Paradigm EarthStudy 360 is
More informationSummary. Introduction
Multivessel coil shooting acquisition with simultaneous sources Nick Moldoveanu¹, Ying Ji², Craig Beasley¹ ¹WesternGeco, ²Schlumberger Cambridge Research Summary Multivessel coil shooting is a towed-streamer
More informationThe Effect of a Dipping Layer on a Reflected Seismic Signal.
The Effect of a Dipping Layer on a Reflected Seismic Signal. Edward O. Osagie, Ph.D. Lane College, Jackson, TN 38305 E-mail: eosagiee@yahoo.com ABSTRACT Modern seismic reflection prospecting is based on
More informationRefraction Full-waveform Inversion in a Shallow Water Environment
Refraction Full-waveform Inversion in a Shallow Water Environment Z. Zou* (PGS), J. Ramos-Martínez (PGS), S. Kelly (PGS), G. Ronholt (PGS), L.T. Langlo (PGS), A. Valenciano Mavilio (PGS), N. Chemingui
More informationIntroduction to the traveltime tomography and prestack migration for borehole-data within REFLEXW
Introduction to the traveltime tomography and prestack migration for borehole-data within REFLEXW In the following the use of the traveltime tomography and the prestack-migration for different types of
More informationImproved Imaging through Pre-stack Trace Interpolation for missing offsets of OBC data A case study from North Tapti area of West Coast, India
P-256 Improved Imaging through Pre-stack Trace Interpolation for missing offsets of OBC data A case study from North Tapti area of West Coast, India M Lal, CPS Rana, Ramji Pathak, BN Bhatta, DP Sinha,
More informationGeogiga Seismic Pro 8.3 Release Notes
Geogiga Seismic Pro 8.3 Release Notes Copyright 2017, All rights reserved. Table of Contents Introduction...1 Part 1 Utility Modules...2 Part 2 Reflection Modules...4 Updates in SF Imager...5 Updates in
More informationRobustness of the scalar elastic imaging condition for converted waves
CWP-830 Robustness of the scalar elastic imaging condition for converted waves Yuting Duan & Paul Sava Center for Wave Phenomena, Colorado School of Mines ABSTRACT For elastic reverse-time migration, one
More informationDownward propagation: using true near-surface velocity model, one-way wave- equation extrapolator:
Class 9: Beyond Seismic Statics Corrections Wed, Oct 7, 2009 Dynamic corrections: wave-equation and wavefield datuming methods Skipping the near-surface by interferometry (no model needed) Common-Focus
More informationH003 Deriving 3D Q Models from Surface Seismic Data Using Attenuated Traveltime Tomography
H003 Deriving 3D Q Models from Surface Seismic Data Using Attenuated Traveltime Tomography M. Cavalca* (Schlumberger - Westerngeco) & R.P. Fletcher (Schlumberger - Westerngeco) SUMMARY Estimation of the
More informationSeismic Reflection Method
Seismic Reflection Method 1/GPH221L9 I. Introduction and General considerations Seismic reflection is the most widely used geophysical technique. It can be used to derive important details about the geometry
More informationMultichannel deconvolution imaging condition for shot-profile migration
Stanford Exploration Project, Report 113, July 8, 2003, pages 127 139 Multichannel deconvolution imaging condition for shot-profile migration Alejandro A. Valenciano and Biondo Biondi 1 ABSTRACT A significant
More informationImaging and Full Waveform Inversion of seismic data from the CO 2 gas cloud at Sleipner
Imaging and Full Waveform Inversion of seismic data from the CO 2 gas cloud at Sleipner Espen Birger Raknes, Børge Arntsen, and Wiktor Weibull Norwegian University of Science and Technology (NTNU) Department
More informationNumerical modeling of shear-wave splitting and azimuthal velocity analysis in fractured media
Shear-wave splitting analysis Numerical modeling of shear-wave splitting and azimuthal velocity analysis in fractured media Zimin Zhang, Don C. Lawton, and Robert R. Stewart ABSTRACT This report presents
More informationThe Lesueur, SW Hub: Improving seismic response and attributes. Final Report
The Lesueur, SW Hub: Improving seismic response and attributes. Final Report ANLEC R&D Project 7-0115-0241 Boris Gurevich, Stanislav Glubokovskikh, Marina Pervukhina, Lionel Esteban, Tobias M. Müller,
More informationP071 Land Data Regularization and Interpolation Using Azimuth Moveout (AMO)
P071 Land Data Regularization and Interpolation Using Azimuth Moveout (AMO) A.M. Popovici* (3DGeo Development Inc.), S. Crawley (3DGeo), D. Bevc (3DGeo) & D. Negut (Arcis Processing) SUMMARY Azimuth Moveout
More informationAn implementable alternate survey geometry design for ideal Land 3D Seismic Acquisition
P-093 Summary An implementable alternate survey geometry design for ideal Land Hanuman Sastry Maduri*, Agarwal D.N., ONGC Different 3D Acquisition Geometries are used on land for acquiring 3D Seismic Data
More informationAdaptive Waveform Inversion: Theory Mike Warner*, Imperial College London, and Lluís Guasch, Sub Salt Solutions Limited
Adaptive Waveform Inversion: Theory Mike Warner*, Imperial College London, and Lluís Guasch, Sub Salt Solutions Limited Summary We present a new method for performing full-waveform inversion that appears
More informationPlanning Land 3-D Seismic Surveys
Planning Land 3-D Seismic Surveys Andreas Cordsen, Mike Galbraith, and John Peirce Edited by Bob A. Hardage Series Editor: Stephen J. Hill Geophysical Developments Series No. 9 Society of Exploration Geophysicists
More informationFracture characterization through the use of azimuthally sectored attribute volumes
Fracture characterization through the use of azimuthally sectored attribute volumes Amanda Thompson* and Jamie Rich, Devon Energy Co. Mike Ammerman, Ammerman Geophysical Summary Azimuthal volumes have
More informationSeisTool Seismic - Rock Physics Tool
SeisTool Seismic - Rock Physics Tool info@traceseis.com Supports Exploration and Development Geoscientists in identifying or characterizing reservoir properties from seismic data. Reduces chance of user
More informationA Novel 3-D De-multiple Workflow for Shallow Water Environments - a Case Study from the Brage field, North Sea
A Novel 3-D De-multiple Workflow for Shallow Water Environments - a Case Study from the Brage field, North Sea J. Oukili* (PGS), T. Jokisch (PGS), A. Pankov (PGS), B. Farmani (PGS), G. Ronhølt (PGS), Ø.
More informationTu N Maximising the Value of Seismic Data for Continued Mature Field Development in the East Shetland Basin
Tu N103 16 Maximising the Value of Seismic Data for Continued Mature Field Development in the East Shetland Basin P. Mitchell (TAQA Bratani Limited), J. Raffle* (ION GXT), P. Brown (ION GXT), I. Humberstone
More informationElastic full waveform Inversion for land walkaway VSP data
Elastic full waveform Inversion for land walkaway VSP data Olga Podgornova, Scott Leaney, arwan Charara, Schlumberger; Eric von Lunen, Nexen Energy ULC Summary Full waveform inversion (FWI) is capable
More informationWave-equation migration from topography: Imaging Husky
Stanford Exploration Project, Report 123, October 31, 2005, pages 49 56 Short Note Wave-equation migration from topography: Imaging Husky Jeff Shragge 1 INTRODUCTION Imaging land seismic data is wrought
More informationSeismic Data Preconditioning for Improved Reservoir Characterization (Inversion and Fracture Analysis)
Seismic Data Preconditioning for Improved Reservoir Characterization (Inversion and Fracture Analysis) Darren Schmidt *, Hampson-Russell, Calgary, AB, Canada Darren.Schmidt@cggveritas.com Alicia Veronesi,
More informationSeismic Modeling, Migration and Velocity Inversion
Seismic Modeling, Migration and Velocity Inversion Aliasing Bee Bednar Panorama Technologies, Inc. 14811 St Marys Lane, Suite 150 Houston TX 77079 May 16, 2014 Bee Bednar (Panorama Technologies) Seismic
More informationReflection Seismic Processing
Reflection Seismic Processing Objective Processing Systems General concept of CMP processing Processing Tools SEGY and similar file formats General features of ProMAX Reading: ProMAX manual (Introduction)
More informationNORSAR-3D. Predict and Understand Seismic. Exploring the Earth. Find the answers with NORSAR-3D seismic ray-modelling
Exploring the Earth NORSAR-3D Predict and Understand Seismic Is undershooting possible? Which is the best survey geometry? MAZ, WAZ, RAZ, Coil, OBS? Why are there shadow zones? Can they be illuminated?
More informationBuilding starting model for full waveform inversion from wide-aperture data by stereotomography
Building starting model for full waveform inversion from wide-aperture data by stereotomography Vincent Prieux 1, G. Lambaré 2, S. Operto 1 and Jean Virieux 3 1 Géosciences Azur - CNRS - UNSA, France;
More informationEffects of multi-scale velocity heterogeneities on wave-equation migration Yong Ma and Paul Sava, Center for Wave Phenomena, Colorado School of Mines
Effects of multi-scale velocity heterogeneities on wave-equation migration Yong Ma and Paul Sava, Center for Wave Phenomena, Colorado School of Mines SUMMARY Velocity models used for wavefield-based seismic
More informationEnhanced Imaging of Subsurface by Pre-Stack Merging of Multi-Vintage 3D Data Sets and its Prestack Time Migration A Case Study
P - 255 Enhanced Imaging of Subsurface by Pre-Stack Merging of Multi-Vintage 3D Data Sets and its Prestack Time Migration A Case Study A.K.Bhakta*, ONGC Ltd., India; B.K.Gogoi, ONGC Ltd., India; and Kailash
More information1D internal multiple prediction in a multidimensional world: errors and recommendations
1D internal multiple prediction 1D internal multiple prediction in a multidimensional world: errors and recommendations Pan Pan and Kris Innanen ABSTRACT Internal multiples are more difficult to estimate
More informationCrosswell Imaging by 2-D Prestack Wavepath Migration
Crosswell Imaging by 2-D Prestack Wavepath Migration Hongchuan Sun ABSTRACT Prestack wavepath migration (WM) is applied to 2-D synthetic crosswell data, and the migrated images are compared to those from
More informationMiVu. Microseismic Processing System SURVEY DESIGN SIGNAL PROCESSING EVENT LOCATION VISUALIZATION.
MiVu Microseismic Processing System SURVEY DESIGN SIGNAL PROCESSING EVENT LOCATION VISUALIZATION MiVuTM Microseismic Processing System MiVuTM is a software package designed to perform microseismic monitoring
More informationSubsalt steep dip imaging study with 3D acoustic modeling Lei Zhuo* and Chu-Ong Ting, CGGVeritas
Lei Zhuo* and Chu-Ong Ting, CGGVeritas Summary We present a 3D acoustic wave equation modeling study with the objective of understanding imaging challenges for steep dips (faults and three-way closure)
More informationSimultaneous joint inversion of refracted and surface waves Simone Re *, Claudio Strobbia, Michele De Stefano and Massimo Virgilio - WesternGeco
Simultaneous joint inversion of refracted and surface waves Simone Re *, Claudio Strobbia, Michele De Stefano and Massimo Virgilio - WesternGeco Summary In this paper, we review the near-surface challenges
More informationRadExPro release notes
1 RadExPro 2017.3 release notes We are excited to tell you that RadExPro 2017.3 is ready now. There is a lot of useful new features in this release: Brand-new Acoustic Inversion module implements a genetic
More information2010 SEG SEG Denver 2010 Annual Meeting
Localized anisotropic tomography with checkshot : Gulf of Mexico case study Andrey Bakulin*, Yangjun (Kevin) Liu, Olga Zdraveva, WesternGeco/Schlumberger Summary Borehole information must be used to build
More informationSeismic Time Processing. The Basis for Modern Seismic Exploration
The Future of E&P Seismic Time Processing The Basis for Modern Seismic Exploration Fusion is a leading provider of Seismic Processing for the oil and gas industry from field tapes through final migration.
More informationIntegral equation method for anisotropic inversion of towed streamer EM data: theory and application for the TWOP survey
Integral equation method for anisotropic inversion of towed streamer EM data: theory and application for the TWOP survey Michael S. Zhdanov 1,2, Masashi Endo 1, Daeung Yoon 1,2, Johan Mattsson 3, and Jonathan
More informationBob Hardage 1. Search and Discovery Article #40662 (2010) Posted December 17, Shallowest Target and Line Spacings
GC 3-D Design Philosophy Part 2: Target Depth* Bob Hardage 1 Search and Discovery Article #40662 (2010) Posted December 17, 2010 *Adapted from the Geophysical Corner column, prepared by the author, in
More informationClosing the Loop via Scenario Modeling in a Time-Lapse Study of an EOR Target in Oman
Closing the Loop via Scenario Modeling in a Time-Lapse Study of an EOR Target in Oman Tania Mukherjee *(University of Houston), Kurang Mehta, Jorge Lopez (Shell International Exploration and Production
More informationTu STZ1 06 Looking Beyond Surface Multiple Predictions - A Demultiple Workflow for the Culzean High Density OBC Survey
Tu STZ1 06 Looking Beyond Surface Multiple Predictions - A Demultiple Workflow for the Culzean High Density OBC Survey S. Gupta (Schlumberger), A. Merry (Maersk Oil), L.P. Jensen (Maersk Oil), A. Clarke
More informationDip or Strike? Complementing geophysical sampling requirements and acquisition efficiency
Dip or Strike? Complementing geophysical sampling requirements and acquisition efficiency Sandeep K Chandola 1*, Low Cheng Foo 1, M Nabil El Kady 1, Thomas Olanrenwaju Ajewole 1, Satyabrata Nayak 1, M
More informationSUMMARY ELASTIC SCALAR IMAGING CONDITION
Robust 3D scalar imaging condition for elastic RTM Yuting Duan, presently at Shell International Exploration and Production Inc., formerly at Center for Wave Phenomena, Colorado School of Mines Paul Sava,
More informationAzimuth Moveout (AMO) for data regularization and interpolation. Application to shallow resource plays in Western Canada
Azimuth Moveout (AMO) for data regularization and interpolation. Application to shallow resource plays in Western Canada Dan Negut, Samo Cilensek, Arcis Processing, Alexander M. Popovici, Sean Crawley,
More informationShot-based pre-processing solutions for wide azimuth towed streamer datasets
first break volume 25, March 2007 focus on azimuth Shot-based pre-processing solutions for wide azimuth towed streamer datasets Philippe Herrmann, 1* Gordon Poole, 2 Antonio Pica, 1 Sylvain Le Roy, 1 and
More informationControlled stacking for improved quality of prestack depth-migration results
CORNER INTERPRETER S Controlled stacking for improved quality of prestack depth-migration results DAVID KESSLER, CGG American Services, Houston, Texas LUIS CANALES and CHUNG-CHI SHIH, CogniSeis Development,
More informationG009 Multi-dimensional Coherency Driven Denoising of Irregular Data
G009 Multi-dimensional Coherency Driven Denoising of Irregular Data G. Poole* (CGGVeritas Services (UK) Ltd) SUMMARY Many land and ocean bottom datasets suffer from high levels of noise which make the
More informationTomoXPro. Crosshole Survey Design, Modeling, Data Processing, Tomography, and Migration
TomoXPro Crosshole Survey Design, Modeling, Data Processing, Tomography, and Migration TomoXPro Complete Crosshole Seismic Application Crosshole survey design for complex geology Synthetic and wavefield
More informationWe LHR5 06 Multi-dimensional Seismic Data Decomposition for Improved Diffraction Imaging and High Resolution Interpretation
We LHR5 06 Multi-dimensional Seismic Data Decomposition for Improved Diffraction Imaging and High Resolution Interpretation G. Yelin (Paradigm), B. de Ribet* (Paradigm), Y. Serfaty (Paradigm) & D. Chase
More informationE044 Ray-based Tomography for Q Estimation and Q Compensation in Complex Media
E044 Ray-based Tomography for Q Estimation and Q Compensation in Complex Media M. Cavalca* (WesternGeco), I. Moore (WesternGeco), L. Zhang (WesternGeco), S.L. Ng (WesternGeco), R.P. Fletcher (WesternGeco)
More informationExamples of GLOBE Claritas Processing
V6.0 Examples of GLOBE Claritas Processing Refraction Statics Removal of Noise (Land, 3D) Removal of Swell Noise Interpolation : shots/receivers Interpolation : 5D (STITCH) Demultiple : High Resolution
More informationUsing Similarity Attribute as a Quality Control Tool in 5D Interpolation
Using Similarity Attribute as a Quality Control Tool in 5D Interpolation Muyi Kola-Ojo Launch Out Geophysical Services, Calgary, Alberta, Canada Summary Seismic attributes in the last two decades have
More informationGG450 4/5/2010. Today s material comes from p and in the text book. Please read and understand all of this material!
GG450 April 6, 2010 Seismic Reflection I Today s material comes from p. 32-33 and 81-116 in the text book. Please read and understand all of this material! Back to seismic waves Last week we talked about
More informationGeOlympus. GeoPACS GeoTR GeoStaR GeoWZ
GeOlympus GeoPACS GeoTR GeoStaR GeoWZ GeOlympus Workstation Work station Reflection time Refracted waves first arrivals Additional information Static and NMO corrections Layer by layer delay and statics
More informationWe N Depth Domain Inversion Case Study in Complex Subsalt Area
We N104 12 Depth Domain Inversion Case Study in Complex Subsalt Area L.P. Letki* (Schlumberger), J. Tang (Schlumberger) & X. Du (Schlumberger) SUMMARY Geophysical reservoir characterisation in a complex
More informationPart 1: Calculating amplitude spectra and seismic wavelets
Geology 554 Environmental and Exploration Geophysics II Generating synthetic seismograms The simple in-class exercise undertaken last time illustrates the relationship between wavelet properties, interval
More informationModeling in Seismic. Tesseral Geo Modeling. Capability to compute 2D-2C and 3D- 3C gathers Enables Geo-scientists to make:
www.tesseral-geo.com Multiparameter Numerical Medium for Seismic Modeling, Planning, Imaging & Interpretation Worldwide Tesseral Geo Modeling Modeling in Seismic Ray-tracing, and especially, finite-difference
More informationMulti-Dimensional Seismic Data Decomposition for Improved Diffraction Imaging and High Resolution Interpretation
Multi-Dimensional Seismic Data Decomposition for Improved Diffraction Imaging and High Resolution Interpretation Bruno de Ribet Technology Global Director Elive Menyoli P&I US Senior Technical Advisor
More information