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GCSeismic Aids Heterogeneity Hunt*
Satinder Chopra1 and Yong Xu2
Search and Discovery Article #40489 (2010)
Posted February 19, 2010
*Adapted from the Geophysical Corner column, prepared by the authors, in AAPG Explorer, November, 2009. Editor of Geophysical Corner is Bob A. Hardage ([email protected]). Managing Editor of AAPG Explorer is Vern Stefanic; Larry Nation is Communications Director.
1Arcis Corp, Calgary, Canada ([email protected])
2previously with Arcis Corp, Calgary, Canada
Canada’s Athabasca oil sands represent the biggest petroleum accumulation in the world and presently produce more than one million barrels of oil per day. These are the Lower Cretaceous bitumen sand reservoirs comprising the McMurray
Formation
that varies in thickness from 10 to 90 meters and occurs at depths of 0 to 400 meters. While the shallow oil sands are exploited by open-pit mining, the deeper reservoirs are produced through some type of insitu bitumen production like SAGD (Steam-Assisted Gravity Drainage).
SAGD operations require extensive, bitumen-saturated, homogeneous formations for optimum production. The McMurray
Formation
, however, is heterogeneous in terms of reservoir continuity, mineralogy, sedimentary facies and
water
-saturation, and is too complex to be fully understood from the sparse available core database. Surface seismic data are one option for characterizing this reservoir heterogeneity, with a common approach being to use neural networks or statistical analysis at well locations to deduce relationships between seismic attributes and lithology. These relationships are then used to determine lateral lithology variations between wells.
uGeneral statement
|
We describe here a two-step approach to understand the heterogeneity of Athabasca oil-sand reservoirs. The first step involves a rock physics study to understand relationships between lithology and petrophysical parameters. From this effort, lithology-sensitive rock parameters are selected that can be detected seismically. The second step is to derive these lithology parameters from seismic data. The first step – rock physics analysis – is carried out for various rock physics parameters across the zone of interest. Parameters that exhibit the best sensitivity to lithology are selected. For example, on Figure 1 we show P-impedance, Vp/Vs velocity ratio and Now that the desired rock parameter – On Figure 2 we show a This study demonstrates the application of rock physics analysis and the determination of rock
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