A Practical Guide to Seismic Fracture Detection Methods

Presented by Mike Perz, VP Technology

Wednesday, June 20, 2012 & Thursday, June 21, 2012
11:45 am—1:00 pm, Lunch Provided

Arcis Seismic Solutions
Centennial Place
3rd Floor, 250—5th Street SW

Fracture estimation via surface-seismic data is enjoying increasing use in resource play exploitation, and this no-nonsense talk is aimed at any practitioner who wants the real dope on how, and whether, seismic fracture detection tools can help them find more pay.

The first part of the talk will focus on the AVAZ and VVAZ methodologies, techniques which exploit azimuthal variations in amplitude and velocity, respectively, in order to estimate fracture properties. The presentation will provide a clear exposition of algorithmic pros and cons, a description of data preparation workflows, and (of supreme importance) a demonstration of the use of quality control metrics during interpretation. The second part of the talk will discuss Arcis’ vision for incorporation of additional fracture detection attributes, specifically those generated by curvature and AVO analysis of P wave data and by shear wave splitting analysis of converted wave data, in order to heighten confidence in interpretation.

 

Spectral Broadening of Multicomponent Data

Presented by Chuck Ursenbach, Senior Research Developer

Wednesday, April 18, 2012
11:45 am—1:00 pm, Lunch Provided

Arcis Seismic Solutions
Centennial Place
3rd Floor, 250—5th Street SW

Perhaps the single most important reason that multicomponent data are not as widely used as vertical P-wave data is the stronger attenuation of S-waves. Accordingly a primary objective in multicomponent processing is to elicit the maximum bandwidth possible from the data.

Two recent studies have brought this subject again to the fore, and have made claims regarding important concepts related to the process of mapping PS data to PP time. In this talk we will consider the validity of these recent studies in the literature and address a number of both basic and advanced questions:

Why do we do PS-to-PP mapping?

What is the best way to perform PS-to-PP mapping?

What determines resolution in PS data?

Are there limits to enhancing the resolution of PS data?

Would such limits be fundamental or just practical?

What are the best methods for enhancing resolution of PS data?

We will describe the steps one must follow to answer these questions, and provide illustrations of the answers.

 

Seismic detection of faults and fractures

Presented by Satinder Chopra, Chief Geophysicist, Reservoir

Wednesday, March 28

11:45 am—1:00 pm, Lunch Provided

Arcis Seismic Solutions
Centennial Place
21st Floor, 250—5th Street SW

Characterization of natural faults and fractures in the subsurface is essential to the design of effective drilling programs and exploitation of tight reservoirs as well as the improved performance of conventional reservoirs. The presence of naturally occurring fracture networks can lead to unpredictable heterogeneity leading to sweet spots and bypassed pay within many reservoirs. If they can be mapped, fractures may provide high permeability pathways that can be exploited to extract reserves stored in a low permeability rock matrix. The need to detect and characterize fractures has motivated the development of new and rejuvenation of older geophysical technologies concerned with or related to fractures. Some of the commonly used methods are the azimuthal AVO method, the use of coherence and curvature seismic attributes, wide azimuth data, multicomponent data and passive seismic techniques. Azimuthal AVO has been used in the industry and has proved to be a promising tool when the assumptions for its application are met. Seismic attributes such as coherence and curvature can be used for both qualitative and quantitative interpretation of fractures. Both these methods will be discussed in the talk. One useful feature, which is not practiced routinely in our industry, is to make use of these two methods together in that unified displays of attributes from these methods should be used for interpretation of fractures.

In general, curvature is an excellent measure of paleo deformation. With an appropriate tectonic deformation model, structural geologists can predict where the fractures were formed. However, since their formation, such fractures may have been cemented, filled with overlying sediments or diagenetically altered. Furthermore, the present-day direction of minimum horizontal stress may have rotated from the direction at the time of deformation, such that previously open fractures are now closed, while previously closed fractures may now be open. For this reason, prediction of open fractures requires not only images of faults and flexures provided by coherence and curvature coupled with an appropriate model of deformation, but also measures of present day stress provided by breakouts seen in image logs and seismic anisotropy measures.

To reach this stage, the input seismic data used for the generation of coherence and curvature attributes should be relatively noise free and should have optimum frequency content for meeting the desired goals. Certain types of noise can be addressed by the interpreter through careful structure-oriented filtering or post migration footprint suppression. Other problems such as multiple contamination or poor imaging due to inaccurate velocities or irregular geometries require that the data go back to the processing team for remediation. Another common problem with seismic data is their relatively low bandwidth. For detection of fractures, the seismic data should have an optimum frequency bandwidth and for this reason frequency enhancement of the input seismic data should be undertaken. I will emphasize the application of a couple of the newer methods for fracture detection. These will include the spectral decomposition-based inversion for seismic reflectivity, a process that removes the time-variant wavelet from the seismic data and extracts the reflectivity to image thicknesses below conventional expectations of seismic resolution. In addition to enhanced images of thin reservoirs, these frequency-enhanced inverse images have proven very useful in mapping subtle onlaps and offlaps, thereby facilitating the mapping of parasequences and the direction of sediment transport.

Finally, I will illustrate some of the latest curvature measures such as Euler curvature for observing fracture lineaments, and structural curvature versus amplitude curvature. Applications of additional recent newer volumetric attributes such as reflector convergence and reflector rotation about the normal to the reflector dip have shown promise and will be touched upon. While the former attribute is useful in the interpretation of angular unconformities, the latter attribute determines the rotation of the fault blocks across discontinuities such as wrench faults. Such attributes can facilitate and quantify the use of seismic for stratigraphic workflows and for large 3D seismic volumes.

CSEG Technical Luncheons - March 14, 2011

   

Extracting Meaningful Information from Seismic Attributes
Satinder Chopra

Telus Convention Centre

8th Ave SE, Calgary

March 14, 2011 - 11:30am

       

Abstract and Bio posted on http://www.cseg.ca/events/luncheons/2011/03mar/20110314-Chopra.cfm

CSEG Technical Luncheons - February 14, 2011

   

Advances in "True Volume" Interpretation of Structure and Stratigraphy in 3D Volumes
Geoffrey A. Dorn

Telus Convention Centre

8th Ave SE, Calgary

February 14, 2011 - 11:30am

     
               

Lunchbox Geophysics - November 23, 2010

Speaker: Mike Perz, Manager, Technology and Integration, Arcis Corporation
Title: Beauty algorithm, eh? (A perspective on Canadian processing innovation)

Time/Date: 12.00 noon, Tuesday, November 23rd, 2010
Place: Aquitaine Auditorium, +15 level of 540 - 5 Avenue SW

 

Abstract and Bio posted on http://www.cseg.ca/events/lunchbox/2010/20101123-Perz.cfm

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