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The AAPG/Datapages Combined Publications Database

Showing 193 Results. Searched 200,293 documents.

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Broad bandwidths reveal double the expected sediment depth in the Northern Carnarvon Basin

Jo Firth, Mark Stanley

Petroleum Exploration Society of Australia (PESA)

... the depth that had been imaged previously, see figure 3. The clear imaging of these deep events was enhanced by sophisticated high-resolution velocity model...

2016

Chapter 3: Preparation of Seismic Data for Stratigraphic Work

Tom Wittick

North Texas Geological Society

... amplitude. The amplitude decays with time due to the spherical spreading of the wavefront. Figure 3-1. Amplitude of a Seismic Trace Notice...

1992

Preparation of Seismic Data For Stratigraphic Work

Abilene Geological Society

... decays with time due to the spherical spreading of the wavefront. Figure 1. Amplitude of a Seismic Trace Notice that there are two components...

1993

Using Multi-Focusing 3-D Diffraction Imaging to Predict Fracture Swarms in Unconventional Reservoirs

Marianne Rauch-Davies, Alex Berkovitch, Kostya Deev

Unconventional Resources Technology Conference (URTEC)

... paraxial wavefront: normal incident point wave and normal wave respectively; X  and X  are the source and receiver offsets for a given X 0 ; R+ and R...

2013

Abstract: The Benefits of S-waves and Multicomponent Data for Surface Monitoring; #90187 (2014)

en Dando, Kit Chambers, Raquel Velasco, and Stephen Wilson

Search and Discovery.com

... source-array geometry by propagating P and S wavefields through 3D P-wave and S-wave velocity models. To compute the synthetics we use a wavefront...

2014

Seismic Models of a Shelf-margin Depositional Sequence: Upper San Andres Formation, Last Chance Canyon, New Mexico

Jan Stafleu , Mark D. Sonnenfeld

Journal of Sedimentary Research (SEPM)

... velocity gradients. The vertical-incidence modeling technique was used to compute perfectly migrated time and depth sections with different frequencies...

1994

3D anisotropic seismic simulation for fracture prediction in Sichuans Wufeng shale gas reservoirs

Xiang Li, Ziduo Hu, Chunhui Xie, Yancan Tian, Wei Liu, Xinyu Fang, Gang Yao

International Meeting for Applied Geoscience and Energy (IMAGE)

... vertically through the source point and the depth slice of the target layer, showcasing P-wave velocity, density, and anisotropic parameters...

2024

Application of Zero Offset 2D CRS-Stack Method for Low Fold Data: Synthetic and Real Data Examples

R. Sule, A. Hendriyana, P. D. Anggraini, Fatkhan, Alfian, Sardjito, Waluyo, Adriansyah

Indonesian Petroleum Association

... velocity model in depth domain. data. This is optimization problem, and one possible approach to determine those attributes is test all attributes...

2009

Practical Application of Adaptive Least-Squares Reverse Time Migration (LSRTM) to Advance Field Development and Uncover New Reserves in the Subsalt Provinces

Chong Zeng, Shuqian Dong, Zhaohong Wu, Jean Ji, Darrell Armentrout, Bin Wang

GCAGS Transactions

... to the requirement of seismic velocity in conventional depth migration algorithms. In theory, LSRTM has to assume the velocity model is perfect otherwise...

2016

An Experimental Investigation of the Anisotropic Dynamic and Static Properties of Eagle Ford Shales

Yang Wang, De-Hua Han, Luanxiao Zhao, Abhijit Mitra, Samir Aldin

Unconventional Resources Technology Conference (URTEC)

... or nearly hydrostatic as the first order to characterize the shale velocity anisotropy (Vernik and Nur, 1992; Vernik and Liu, 1997). However, in most cases...

2019

Abstract: 3D, Anisotropic Phase Shift Operators; #90171 (2013)

Robert J. Ferguson and Gary F. Margrave

Search and Discovery.com

... is acoustic velocity. Unit normal  (2) For numerical wave-propagation in the Fourier domain  k 1, k 2,   , where k 1 a n d k 2 are the  Fourier...

2013

Abstract: 3D, Anisotropic Phase Shift Operators; #90171 (2013)

Robert J. Ferguson and Gary F. Margrave

Search and Discovery.com

... is acoustic velocity. Unit normal  (2) For numerical wave-propagation in the Fourier domain  k 1, k 2,   , where k 1 a n d k 2 are the  Fourier...

2013

Abstract: Separation of Geometric Spreading, Scattering and Intrinsic Attenuation in VSP data; #90187 (2014)

Amin Baharvand Ahmadi and Igor Morozov

Search and Discovery.com

... (blue labels). Table 1: Resulting separated geometric-spreading, scattering and intrinsic-attenuation model* Depth to Velocity -1 -1 -1 Layer v...

2014

Abstract: Using-MultiFocusing 3D Diffraction Imaging to Predict Fracture Corridors/swarms in the Bazhenov Formation; #90187 (2014)

Marianne Rauch-Davies, Alex Berkovitch, Danil Pelman, and Kostya Deev

Search and Discovery.com

...  X    X  X  2 sin  Rcre (3) b is the normal ray; Rcre and Rcee are radii of curvatures of two paraxial wavefront: normal incident point wave...

2014

Impact of an Integrated Seismic Data Processing Approach: A Case Study in Central Sumatra

Mars E. Semaan, Eddy Murhantoro, Maryanto, Achmad Bermawi, Budi Subianto, Hari Santoso

Indonesian Petroleum Association

... velocities and their relationships (Poisson's ratio). The resulting P-wave velocity can be used to perform time-to-depth conversion and to predict target...

1992

Persistent Microseismic Monitoring Using Robust Permanent SADAR Arrays

Kevin D. Hutchenson, Jason Jennings, Elige B. Grant, Derek Quigley, Jonathan Yelton, Paul A. Nyffenegger

Carbon Capture, Utilization and Storage (CCUS)

... at Carbon Management Canada’s Field Research Station (FRS) proving ground between 9m-19m depth to demonstrate passive and activesource seismic...

2025

Seismic Processing Applications on a Personal Computer

Geophysical Service (Malaysia) Sdn. Bhd.

Geological Society of Malaysia (GSM)

... the velocity vs depth relationship for both P-wave and S-wave energy. 60 GEOPHYSICAL SERVICE (M ) Figure 6: SnN. B HD. 2-panel display, upgoing...

1989

Improvement of inverse scattering angle-domain common image gathers using optical flow

Ammir A. Karsou, Sérgio L. E. F. da Silva, Felipe V. Capuzzo, Felipe T. Costa, Jorge Lopez, Roger M. Moreira, Marco Cetale

International Meeting for Applied Geoscience and Energy (IMAGE)

...spacing is 10 m at the depth of 10 m, simulating streamer acquisition. ADCIGs are chosen to display for every 400m in the velocity model which are repr...

2023

Data Enhancement from a 486-Channel Streamer

Bill Dragoset, Ken Larner

Pacific Section of AAPG

... frequency components. The amount of attenuation depends on the velocity distribution, array length and offset, and reflector dip and depth. Figure 5...

1980

Technical Article: Finding Subtle Traps with Seismic: Interpretative Criteria Clarified

A. Easton Wren

Petroleum Exploration Society of Australia (PESA)

... travel time or the depth to the reflecting interface. Such early seismic principles yielded detailed structural data, but geophysical technology...

1986

Geometric and seismic interpretation of the Perdido fold belt: Northwestern deep-water Gulf of Mexico

Rion H. Camerlo, Edward F. Benson

AAPG Bulletin

... that result from this aforementioned poor velocity control, especially with increasing depth. The same relationship can be seen at the level of the deeper...

2006

Where's the Data? Acquisition and Processing of Seismic Data in the PNG Highlands

Subhash Chandra, Geoff Mansfield, Peter Carver

Petroleum Exploration Society of Australia (PESA)

... poor when velocity inversion, and extreme topography. compared to other areas, has been continuously improved over These issues result in the cost...

2015

Chapter 6: Seismic Modeling

Tom Wittick

North Texas Geological Society

... in velocity in the subsurface the raypaths are bent according to Snell’s law so we get the curved raypath. There are two types of ray trace modeling...

1992

Seismic Modeling

Abilene Geological Society

... is a technique which traces the raypath the sound travels going from the shot to the receiver. Wherever there are changes in velocity in the subsurface...

1993

Vertical Seismic Profiling in Hydrocarbon Exploration and Reservoir Development

Bob A. Hardage

Circum Pacific Council Publications

... depth, Z, is depicted on a vertical coordinate axis, and recording time, T, is represented on a horizontal coordinate axis. When plotted in this manner...

1989

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