- Page 1 and 2: June 29, 2006 Seismic Evaluation of
- Page 3 and 4: Abstract: During this last quarter
- Page 5 and 6: Ursa Data .........................
- Page 7 and 8: Figures: Figure 1. Relationship of
- Page 9 and 10: Figure 38. Schematic of geometry an
- Page 11 and 12: Figure 73. The extracted wavelet an
- Page 13 and 14: Executive Summary: In this joint pr
- Page 15 and 16: Results and Discussion Introduction
- Page 17 and 18: Inversion of Sw and porosity from s
- Page 19 and 20: saturation from seismic data. Valid
- Page 21 and 22: The Lagrange function (5) has a sad
- Page 23 and 24: ρ ma − ρ + ( ρ w − ρ g ) ×
- Page 25 and 26: With a water saturation log calcula
- Page 27 and 28: Figure 11. permeability versus poro
- Page 29 and 30: Figure 13. Measured dry and brine s
- Page 31 and 32: Figure 15. The HP (deep) sands have
- Page 33 and 34: pressure-porosity relations. The n
- Page 35 and 36: Figure 19. measure dry and brine sa
- Page 37 and 38: Relations between Sw, porosity, and
- Page 39 and 40: Figure 21. An example realization o
- Page 41 and 42: otherwise the seismic properties we
- Page 43 and 44: correctly reproduce those found in
- Page 45: study of field data from the Teal S
- Page 49 and 50: (Adapted from CSM Slope and Basin C
- Page 51 and 52: Figure 34. Sequence stratigraphic f
- Page 53 and 54: Figure 36. Schematic depiction of c
- Page 55 and 56: Figure 38. Schematic of geometry an
- Page 57 and 58: Figure 40. Middle slope channel (Ad
- Page 59 and 60: Figure 43. Amalgamated sandstone sh
- Page 61 and 62: CHANNEL AXIS SINGLE STORY CHANNEL C
- Page 63 and 64: MEDIAL LEVEE/OVERBANK 7.62 cm Figur
- Page 65 and 66: L1054 L1041 • Ursa Well A4 Green=
- Page 67 and 68: 1.9 miles 37 ft Fizz 19 ft Oil 4.0
- Page 69 and 70: esults in shifts followed by subsid
- Page 71 and 72: Figure 55. Schematic of depositiona
- Page 73 and 74: 4 miles 1.5 s 2 s 3 s Hydrocarbon I
- Page 75 and 76: In addition to comparing calculated
- Page 77 and 78: Figure 61. Shear velocity trend for
- Page 79 and 80: each reservoir interval modeled. Th
- Page 81 and 82: Figure 65. Histograms of frequency
- Page 83 and 84: the pressure trends were analyzed,
- Page 85 and 86: P Impedance Model Synthetic 2 -D Mo
- Page 87 and 88: Above Magenta reservoir model The A
- Page 89 and 90: Figure 73. The extracted wavelet an
- Page 91 and 92: saturation and 50% gas saturation.
- Page 93 and 94: Figure 77. The amalgamated channel
- Page 95 and 96: Figure 79. Channel complex model 2
- Page 97 and 98:
Figure 81. AVO stack and gathers fo
- Page 99 and 100:
Figure 82. Log signature includes g
- Page 101 and 102:
Figure 85. Extracted wavelet and mo
- Page 103 and 104:
Figure 87. Amalgamated sheet sand m
- Page 105 and 106:
Figure 89. Pseudo logs, wavelet, sy
- Page 107 and 108:
Figure 90. Medial basin floor chann
- Page 109 and 110:
Figure 92. Pseudo logs, wavelet, sy
- Page 111 and 112:
Figure 94. The post stack seismic e
- Page 113 and 114:
Figure 96. Statistically extracted
- Page 115 and 116:
Figure 98. The proximal levee overb
- Page 117 and 118:
Figure 99. The response of the prox
- Page 119 and 120:
Figure 101. The pseudo log, wavelet
- Page 121 and 122:
Figure 102. The distal levee overba
- Page 123 and 124:
Figure 104. The complex well log ba
- Page 125 and 126:
then scaled to the model data by mu
- Page 127 and 128:
Figure 107. The Ursa log displays g
- Page 129 and 130:
Figure 109. Composite reflection co
- Page 131 and 132:
Conclusions One of the main conclus
- Page 133 and 134:
Table 5 Summary of the model facies
- Page 135 and 136:
REFERENCES Alford, R. M., Kelly, K.
- Page 137 and 138:
Gardner, M. H., Anderson, D. A., Bo
- Page 139 and 140:
Mahaffie, M.J., 1994, Reservoir cla
- Page 141 and 142:
Rothman, D.H., Grotzinger, J.P., Fl
- Page 143 and 144:
Vail, P., 1977, Seismic Stratigraph
- Page 145 and 146:
downlap (Mtchum, 1977): A base-disc
- Page 147 and 148:
direction and downlap onto the tran
- Page 149 and 150:
Agreement DE-FC26-02NT15342, Seismi
- Page 151 and 152:
Agreement DE-FC26-02NT15342, Seismi
- Page 153 and 154:
Agreement DE-FC26-02NT15342, Seismi
- Page 155 and 156:
Agreement DE-FC26-02NT15342, Seismi
- Page 157 and 158:
Agreement DE-FC26-02NT15342, Seismi
- Page 159 and 160:
APPENDIX E: VALUES USED FOR RESERVO