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

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Table 5.1. Preliminary assessment of wells of <strong>the</strong> sou<strong>the</strong>ast Bowen Basin area.<br />

Well<br />

(north-to-south)<br />

Base of<br />

Precipice<br />

Sandstone (m)<br />

Top of<br />

Permian<br />

Section (m)<br />

Triassic<br />

Reservoir<br />

Potential?<br />

Permian<br />

Reservoir<br />

Potential?<br />

Juandah-1 1457 1994 No No<br />

Gurulmundi-1 1250 Not enough data No No<br />

Dulacca-1 1629 Not enough data Not enough data Not enough data<br />

Auburn-1 1618.5 Not enough data Not enough data Not enough data<br />

Miles-1 1228 Not enough data Not enough data Not enough data<br />

Columboola-1 1167 1185 No Not enough data<br />

Tey-1 1626 1626 No Not enough data<br />

Bennett-1 1714.5 1716 No Not enough data<br />

Undulla-1 1725 1737 No Minor Potential<br />

Leichhardt-1 1771 1790 No Not enough data<br />

Alick Creek-1 Not present 1640 No Minor Potential<br />

Tara-1 Not present 1639 No Not enough data<br />

Cabawin East-1 2384 3194 No Not enough data<br />

Cabawin-1 2326 3007 Minor Potential Minor Potential<br />

Tartha-1 2185 Not enough data No Not enough data<br />

Southwood-1 2082 2249 No No<br />

Cabawin-1 is <strong>the</strong> only well to have intersected a significant hydrocarbon accumulation. There are<br />

several potential sandstone–conglomerate reservoir intervals in <strong>the</strong> Triassic section of <strong>the</strong> well,<br />

which are thicker here than in any o<strong>the</strong>r part of <strong>the</strong> study area (Figure 5.1). These intervals have<br />

better porosity and permeability characteristics than o<strong>the</strong>rs in <strong>the</strong> study area, and are generally<br />

composed of quartz and chert pebbles with minor ash. However, <strong>the</strong>re is doubt about <strong>the</strong> volume<br />

of CO 2 that could be injected since <strong>the</strong>se sandstones have not been intersected in off-set wells.<br />

There are no obvious regional sealing units in this area, however a thickness of poor quality<br />

(in terms of reservoir) Triassic sequence could act as a significant baffle to vertical migration.<br />

Figure 5.1. Generic geological cross-section of <strong>the</strong> sou<strong>the</strong>ast Bowen Basin area. The cross-section shows<br />

distribution and thickness of Permian and Triassic sediments from north-to-south in <strong>the</strong> sou<strong>the</strong>ast Bowen Basin.<br />

Wells from north-to-south: Juandah-1 (also representing Gurulmundi-1, Dulacca-1, Auburn-1), Columboola-1<br />

(also representing Miles-1), Undulla-1 (also representing Tey-1, Bennet-1, Leichhardt-1), Alick Creek-1 (also<br />

representing Tara-1), Cabawin East-1, Cabawin-1, Tartha-1, Southwood-1.<br />

34

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