Read the full report (PDF27.8 MB) - CO2CRC

More documents

Recommendations

Info

Figure 3.4. Sequence Stratigraphy of the Bowen and Surat basins (after Korsch et al., 1998). 20
Figure 3.5. Structure of the Denison Trough. Note: north–south trending grabens which were deformed during the Late Triassic into fault-propagated anticlines (After Elliot 1985). 21
Page 1: Site Specific Studies for Geologica
Page 4 and 5: Cooperative Research Centre for Gre
Page 6 and 7: 5.7. Chapter References ...........
Page 8 and 9: Tables Table 2.1. Physical properti
Page 10 and 11: Figure 6.19. Photograph of Harbour-
Page 13 and 14: Executive Summary The GEODISC progr
Page 15 and 16: 1. Introduction Significant debate
Page 17 and 18: 2. Geographical and Industrial Sett
Page 19 and 20: Figure 2.2. Close-up images of stud
Page 21 and 22: 10000 1000 AOI for carbon dioxide i
Page 23 and 24: l l 145° 150° l Moranbah Long rea
Page 25 and 26: Table 3.1. Summary of the key risk
Page 27 and 28: 3.1.11. Lakefield Basin. The Lakefi
Page 29 and 30: GEODISC concluded that the Drummond
Page 31: The Denison Trough is a western ext
Page 35 and 36: Figure 3.7.Schematic geological cro
Page 37 and 38: • A comprehensive set of wells an
Page 39 and 40: sandstone of the Bundamba Group, Cl
Page 41 and 42: Figure 4.1. Location of all wells u
Page 43 and 44: 5. Bowen Basin Summary Reviews 5.1.
Page 45 and 46: 5.4. Southeast Bowen Basin Study Ar
Page 47 and 48: 5.4.2. Seismic Data Seven horizons
Page 49 and 50: 5.6. Northeast Bowen Basin Study Ar
Page 51 and 52: 6. Southwest Bowen Basin Study Area
Page 53 and 54: Basement (BASE) The BASE horizon is
Page 55 and 56: 6.1.4. Mapping Time structure, dept
Page 57 and 58: Figure 6.1. Seismic sections across
Page 59 and 60: 0 TWT ~ Depth (SRD = 244m) TWT (ms)
Page 61 and 62: Figure 6.7. BANDANNA-to-SHOWGROUNDS
Page 63 and 64: Maps and Basin Fill The Basement to
Page 65 and 66: Showgrounds Sandstone/Snake Creek M
Page 67 and 68: Using this method there is a potent
Page 69 and 70: 6.3.4. X-ray Diffractometry X-ray D
Page 71 and 72: and permeability are sedimentary fa
Page 73 and 74: Cores from wells located on the Wun
Page 75 and 76: Many of the wells in the central pa
Page 77 and 78: Figure 6.24. Core description of th
Page 79 and 80: oreholes. Depositional processes in
Page 81 and 82: Figure 6.30. Photograph of Rednook-
Page 83 and 84:
Figure 6.32. Relative palaeo-water
Page 85 and 86:
associated with the increase in tot
Page 87 and 88:
The interpretation of multiple chan
Page 89 and 90:
Beyond the meandering system, a del
Page 91 and 92:
c) 148°00' 148*20' 148°40' 27°20
Page 93 and 94:
The ductility and compressibility o
Page 95 and 96:
148:30 149:00 149:30 N Depth toTop
Page 97 and 98:
The only recent well with reasonabl
Page 99 and 100:
Rewan Formation- Showgrounds Sandst
Page 101 and 102:
For a simplified model, as used in
Page 103 and 104:
Table 6.5. Reservoir properties. Pr
Page 105 and 106:
6.7.4. Simulation Results Prelimina
Page 107 and 108:
• it is difficult to quantify the
Page 109 and 110:
Brakel et al., (in press), In Korsc
Page 111 and 112:
7. Summary and Implications - South
Page 113 and 114:
8. Recommendations- Southeast Queen
Page 115 and 116:
9. Acknowledgements The project gro
Page 117 and 118:
List of authors Note: (main authors
show all

Read the full report (PDF27.8 MB) - CO2CRC

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

Delete template?

Save as template?