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Figure 3.6. Key structural elements of the Taroom Trough (after Rigby, 1987). 22
Figure 3.7.Schematic geological cross-section through the Roma Shelf area. Located in the western Taroom Trough showing structural relationships. The Wunger Ridge fields (right hand side) have been projected approximately 60 km north onto cross-section. The distribution of oil and gas fields is shown relative to pinchouts and erosional edges and occurs above Permian source rocks (from Cadman et al., 1998). Arrows indicate hydrocarbon migration pathways and show how hydrocarbons leak up through the formations, creating stacked accumulations. 23
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 and 32: The Denison Trough is a western ext
Page 33: Figure 3.5. Structure of the Deniso
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
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