Application of Inversion and Clustering Analysis in Unconventional Reservoirs

29 September, 2011
Who Should Attend
Geologists, Engineers, Geophysicists, and any Geoscientist, of all experience levels - anyone interested in developing new ways to prospect for sweet spots in unconventional reservoirs.
Objectives
Course Content

Based upon recent studies of the Barnett Shale in Texas, a systematic characterization workflow is necessary to do an accurate reservoir characterization. This should incorporate different tools such as: litho- and sequence-stratigraphy, geochemistry, petrophysics, geomechanics, well log, and 3D seismic analysis. This study will focus in the combination of λρ – μρ inversion with clustering analysis techniques in order to discriminate brittle zones in the Barnett Shale.

3D seismic characterization includes structural and stratigraphic mapping using seismic attributes; calibrating seismic characteristics to lithofacies and gamma ray parasequences (GRP’s) for seismic mapping purposes; and determining and mapping petrophysical properties using seismic inversion modeling. GRP gives us a good understanding of the depositional environment of the shale. On the other hand, petrofacies show the mechanical behavior of the rock in reservoir conditions. Clustering the vertical sequence will allow us to estimate the spatial distribution of the petrofacies.

On the other hand, post-stack seismic inversion was proving to be a very useful tool in order to enhance the seismic resolution of the internal reflectors in the Barnett Shale (Perez, 2008). The objective is to integrate analyzed properties into a geologically-realistic 3D stratigraphic model to better understand the fine-scale stratigraphy of shales and as an aid to improved horizontal well placement. Preliminary results show that the optimum gas shale properties have relatively low λ’s (incompressibility) and high µ’s (rigidity) that give rise to geo-mechanical brittleness capable of supporting extensive induced fractures. These results will be focus in the mechanical properties of the rock, instead of the depositional environment. Plotting λ vs. Young's modulus allows discrimination between ductile and brittle shales in the area of study (Goodway, 2007). Comparing these results and the clustering analysis, we will be able to discriminate different production zones, and correlate these results with the zones having the best petrophysical and mechanical properties (TOC, porosity and permeability).

Structure of the E-Symposium

Each e-symposium consists of one-hour live e-symposium, along with material for one full day of independent study. The live portion will be followed by a full day of independent study (not a live event). The one-hour live e-symposium can be accessed from any computer anywhere in the world using a high-speed internet connection. After the event is over, you will receive via email information about accessing the asynchronous segment (not live) which consists of your independent study materials, to be accessed and studied at any time. You will be able to email responses to the readings, along with your study question answers for CEU credit (if you sign up for the extended package).

Recording of original webinar, packet of independent study reading materials, PDF of original PowerPoint presentation by FTP download. (Original presentation date: September 29, 2011.) Some materials will also sent by e-mail.

$75
$75
Expires on
01 January, 9999
Member Tuition without CEU
$95
$95
Expires on
01 January, 9999
Nonmember Tuition without CEU
$25
$25
Expires on
01 January, 9999
Student Tuition without CEU
$100
$100
Expires on
01 January, 9999
Member Tuition with CEU
$145
$145
Expires on
01 January, 9999
Nonmember Tuition with CEU
$35
$35
Expires on
01 January, 9999
Student Tuition with CEU
200
Limit
1.0
CEU

Expanded package for CEU credit is $100 for AAPG members, and $145 for non-members. Special Student Pricing: $25 for Webinar only; $35 for Expanded package.

 

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Susan Nash, Ph.D. Director of Education and Professional Development +1 918 560 2604
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