29.04.2014 Views

Agreement DE-FC26-02NT15342, Seismic Evaluation of ...

Agreement DE-FC26-02NT15342, Seismic Evaluation of ...

Agreement DE-FC26-02NT15342, Seismic Evaluation of ...

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Figures:<br />

Figure 1. Relationship <strong>of</strong> various rock and fluid properties important for Direct<br />

Hydrocarbon Indicators. ........................................................................................... 15<br />

Figure 2. Test Sites, Gulf <strong>of</strong> Mexico ………………………………………………... 16<br />

Figure 3. Workflow: Conventional and new for Sw and poroosityinversion………… 17<br />

Figure 4. Velocity versus pressure and modulus versus pressure..................................... 18<br />

Figure 5. The s<strong>of</strong>t margin loss setting for a linear SVM (from Smola and Scolkopf, 2004)<br />

................................................................................................................................... 20<br />

Figure 6. The saturation logs (original and regressed from seismic trace with SVM). .... 23<br />

Figure 8. The cross sections <strong>of</strong> estimated water saturation from King Kong (left) and Lisa<br />

Anne (right)............................................................................................................... 24<br />

Figure 9. Dry-bulk and grain density as a function <strong>of</strong> porosity for the shallow (12000 ft)<br />

and deep (17700 ft ) sands ........................................................................................ 26<br />

Figure 10. thin section for a deepwater clean unconsolidated fine sand sample. ............. 26<br />

Figure 11. permeability versus porosity for the shallow and deep sands and shales........ 27<br />

Figure 12. Total pore volume reduction is around 1.5% porosity unit for deepwater sands<br />

with no relation to porosity. There is much high porosity reduction for shaley sands<br />

and shales.................................................................................................................. 28<br />

Figure 13. Measured dry and brine saturated P and S wave velocities on a typical<br />

deepwater sand sample (for about 12, 000 ft) as function <strong>of</strong> differential pressure... 29<br />

Figure 14. (a) measured dry Vp versus porosity . (b) Measured dry Vs versus porosity. 30<br />

Figure 15. The HP (deep) sands have much higher shear modulus than those <strong>of</strong> the VHP<br />

(shallow) sands.......................................................................................................... 31<br />

Figure 16. Measured dry and brine saturated bulk and shear modulus <strong>of</strong> BHP sand<br />

samples in comparison to modulus calculated with Gassmanns’s equation............. 31<br />

Figure 17. Derived gain function porosity. Low bound <strong>of</strong> the gain function for deepwater<br />

sands is around 2.5.................................................................................................... 34<br />

Figure 18. Water saturated P- and S- wave velocity versus porosity with modeled<br />

velocity/porosity trend. ............................................................................................. 34<br />

Figure 19. measure dry and brine saturated Vp/Vs ratio for the shallow VHP and deep HP<br />

sands.......................................................................................................................... 35<br />

Figure 20. Pore fluid bulk modulus for wet and gas formation derived from log data. ... 35<br />

Figure 21. An example realization <strong>of</strong> each <strong>of</strong> the model types, one without spatial<br />

correlation, and two with the von Karman and Gaussian spatial correlations defined<br />

in the text................................................................................................................... 39<br />

Figure 22. Statistics <strong>of</strong> the reflection coefficients for composite reflection coefficients<br />

generated using the three spatial correlation functions and for the Backus average<br />

versions <strong>of</strong> each model. In each case, 50 realizations were considered. Error bars<br />

corresponding to one standard deviation are displayed for the stochastic models,<br />

though not for Backus average results which have negligible scatter on the scale <strong>of</strong><br />

these plots.................................................................................................................. 40<br />

Figure 23. AVO parameters, the intercept and gradient, displayed for each <strong>of</strong> the three<br />

classes <strong>of</strong> models for which we computed composite reflection coefficients. ......... 41<br />

<strong>Agreement</strong> <strong>DE</strong>-<strong>FC26</strong>-<strong>02NT15342</strong>, <strong>Seismic</strong> <strong>Evaluation</strong> <strong>of</strong> Hydrocarbon Saturation 7

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!