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The AAPG/Datapages Combined Publications Database
Showing 32,067 Results. Searched 196,121 documents.
Evaluation of Eustasy, Subsidence, and Sediment Input as Controls on Depositional Sequence Geometries and the Synchroneity of Sequence Boundaries: Chapter 13: Recent Developments in Siliciclastic Sequence Stratigraphy
David T. Lawrence
AAPG Special Volumes
... models are summarized in Table 2. Case 1 (Figure 3) is a model of stratigraphy in a subsiding basin with constant sea level. Subsidence rates increase...
1993
Fines Migration during Coal Bed Methane Production: Mathematical and Laboratory Modelling, Field Cases
Abolfazl Hashemi, Bryant Dang-Le, Cuong Nguyen, Grace Loi, Nastaran Khazali
Australian Petroleum Production & Exploration Association (APPEA) Journal
...Fines Migration during Coal Bed Methane Production: Mathematical and Laboratory Modelling, Field Cases Abolfazl Hashemi, Bryant Dang-Le, Cuong Nguyen...
2023
Seismic Time to Depth Conversion and Uncertainty Analysis for Horizon Prediction in a Proposed Well-Site of Sungai Gelam Field, Jambi Subbasin
Muhamad Wildan P., Imam Muda Gunawan, Andry Pujiriyanto, Sudarmaji
Indonesian Petroleum Association
... depending on the purpose and the availability of existing data sources. In seismic data, processing in the form of migration also involves velocity modeling...
2013
Abstract: Common Reflection Angle Pre-Stack Depth Migration as Data Enhancement Method for 3D Sparse Land Seismic Data, Case Study from Saudi Arabia; #90319 (2018)
Asaad E. Alzawwad, Krzysztof K. Sliz, Luke LaFreniere
Search and Discovery.com
...Abstract: Common Reflection Angle Pre-Stack Depth Migration as Data Enhancement Method for 3D Sparse Land Seismic Data, Case Study from Saudi Arabia...
2018
Sedimentologic and Physical Oceanographic Evidence of a Shelf Edge Counter Current Off Guinea Bissau, Guinea and Sierra Leone
David W. McGrail
Journal of Sedimentary Research (SEPM)
...]/[vx]i + [v]/[vy]j + [v]/[vz]k) a differential operator = (wk) the constant angular velocity of the system i, j, k = unit vectors in the rotating frame...
1977
ABSTRACT: Influence of Salt Geometry and Salt-Sediment Interaction on Seismic Imaging, by Bui, Huyen; Jamieson, George; Snyder, Fred; Herbert, Sharlene; Becker, David; Smith, Martiris; #90135 (2011)
Search and Discovery.com
2011
Gabor Depth Migration using a New Adaptive Partitioning Algorithm
Yongwang Ma
Search and Discovery.com
... created by the algorithm. Gabor Depth Migration Example The Marmousi velocity section used in Gabor depth imaging in this paper is shown in Figure 3...
Unknown
Gabor Depth Migration using a New Adaptive Partitioning Algorithm
Yongwang Ma
Search and Discovery.com
... created by the algorithm. Gabor Depth Migration Example The Marmousi velocity section used in Gabor depth imaging in this paper is shown in Figure 3...
Unknown
Seismic Migration Interpolation using Time-Shift Imaging Condition
Mark Ng
Search and Discovery.com
... variable space and time lag imaging methods, have been used for depthfocusing analysis (DFA) for migration velocity analysis (MacKay and Abma, 1992...
Unknown
Seismic Migration Interpolation using Time-Shift Imaging Condition
Mark Ng
Search and Discovery.com
... variable space and time lag imaging methods, have been used for depthfocusing analysis (DFA) for migration velocity analysis (MacKay and Abma, 1992...
Unknown
Serang Field – Discovery Within a Seismic "Fault Shadow"
Tom Clark, Mike Turk, Joewono Hadiwijoto, Yoseph Partono
Indonesian Petroleum Association
... is partially occluded by a classic fault shadow. A velocity model was used to predict the magnitude and extent of this rather large anomaly resulting...
2000
Velocity-depth trends in Mesozoic and Cenozoic sediments from the Norwegian Shelf
Vidar Storvoll, Knut Bjrlykke, Nazmul H. Mondol
AAPG Bulletin
...-Owe, K. Bjrlykke, R. Olstad, K. Berge, M. Cecchi, E. Vik, and R. G. Schaefer, 2004, Petroleum migration, faults and overpressure: Part II. Case...
2005
III. Evidence of Faulting
Robert E. Sheriff
AAPG Special Volumes
... of seismic lines: (1) Abrupt termination of reflections, especially after migration. Fig. 48. Seismic lines shot over the model shown in Fig. 47. (a) Line...
1981
Abstract: Carbonate Fracture Case History from Russia and Implications for HTD Plays in North America; #90172 (2014)
Inga Khromova, Brian Link
Search and Discovery.com
... case and Lower Devonian in the second case), despite the fact that porosity is almost constant. Numerous thorough investigations have shown...
2014
Rock-Water Reaction: Formation Damage: Part 5. Laboratory Methods
Dare Keelan, J. O. Amaefule
AAPG Special Volumes
... The critical interstitial velocity at which permeability reduction due to fines migration is initiated can be determined in laboratory tests. These tests...
1992
A Regional Velocity Cube for Depth Conversion on the Northwest Shelf
Maighréad Ní Dheasúna, Mark Ballesteros, James Leven
Petroleum Exploration Society of Australia (PESA)
... depth migration (PSDM) is used, or if the velocity model for an anisotropic PSDM does not correctly account for anisotropy, it may be desirable...
2012
Seismic Processing Strategies in the Deep Water Kutai Basin Gendalo Hub Pre-Stack Depth Migration
Xiuyuan Li, Harmit Singh, Joe Zhou, Graham Hodgkiss, Neil Young, Helmut Hsiao
Indonesian Petroleum Association
... as was evident in the imprint of residual velocity error and channeling effect in the Gamma attribute (ratio between migration velocity and true velocity...
2011
Complex Model Building using Objective Construction of Curve Ray Time Migration Moveout with Geologic Constraints, #41596 (2015).
Kerry Stinson, Shlomo Levy, Edward Crase, Wai-Kin Chan
Search and Discovery.com
... Modeling Inc., Calgary, AB, Canada ([email protected]) Abstract A time domain system for high density, high resolution migration velocity estimation...
2015
Competence of Fine-grained Debris Flows
Monty A. Hampton
Journal of Sedimentary Research (SEPM)
.... Integrating equation 9 gives the velocity in the zones of shear: U=[1]/[][[( sin )]/[2]y2-(i+k)y+C1] (10) where C1 is a constant of integration. The velocity...
1975
Wave-Formed Sedimentary StructuresA Conceptual Model
H. Edward Clifton
Special Publications of SEPM
... Geological Survey California 94025 ABSTRACT produced by shoaling waves can be integrated into a conceptual model based on velocity um velocity asymmetry d...
1987
Interpretation Methods in the Exploration of Oligocene-Miocene Carbonate Reservoirs, Offshore Northwest Madura, Indonesia
David C. Carter, Dwi Mandhiri, Robert K. Park, Imron Asjhari, Syaiful Basyuni, Sergey Birdus, John P. Bradfield, Ary Iriawan, Meutia Nasfiah, M.A. Agung Nugroho
Indonesian Petroleum Association
... migration (PSDM), and horizon-based seismic tomography (Kosloff et al., 1996; Yilmas, 2000) is a process that can provide reliable velocity estimates...
2005
Quantitative Assessment of Hydrocarbon Charge Risk in New Ventures Exploration: Are We Fooling Ourselves?
Noelle B. Schoellkopf
AAPG Special Volumes
... models on fetch area and charge. Velocity model 2 removes the dip reversal, allowing a larger fetch area (light gray) and continuous migration. Model...
2012
Limitations on Resolution of Seismic Reflections and Geologic Detail Derivable from Them: Section 1. Fundamentals of Stratigraphic Interpretation of Seismic Data
Robert E. Sheriff
AAPG Special Volumes
... geology. Velocity filtering and the redundancy provided by recording with high degrees of multiplicity permit the attenuation of many types...
1977
Combined Diving Wave Refraction Tomography and Reflection Tomography for PSDM Velocity Model Building (Bekapai Field, Indonesia)
Andi Kusuma, Florent Bertini, Jacques Bonnafe, Artem Sazykin, Swee Leng Ng
Indonesian Petroleum Association
... of near angle information in shallow depths as well as weak transmitted signals in deeper intervals. In our case, the velocity model building process...
2011
Constraints on Eolian Grain Flow Dynamics Through Laboratory Experiments on Sand Slopes
Richard R. McDonald , Robert S. Anderson
Journal of Sedimentary Research (SEPM)
...]/[dvt] + u[dvu]/[dvx] = g sin(q) + g cos(q)[5]/[4]tan(fo)[1 - [1]/[5]exp(-0.64u/ghe)]. (4) The steady-state velocity in this case becomes u = -ln[[-4...
1996