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Geothermal Energy Potential in Selected Areas of Western Australia ...

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11<br />

basement contour maps presented by Iasky (1994) 6 . All available data suggest that<br />

Palaeozoic basement reaches a maximum depth <strong>of</strong> >13 km <strong>in</strong> the Perth Bas<strong>in</strong>.<br />

3.2. Basement Lithology<br />

The basement underly<strong>in</strong>g the Perth Bas<strong>in</strong> is comprised primarily <strong>of</strong> Proterozoic<br />

granulites, gneisses, metasediments and granite <strong>in</strong>trusions <strong>of</strong> the P<strong>in</strong>jarra Orogen.<br />

Basement outcrops can be seen <strong>in</strong> fault bounded mid-bas<strong>in</strong> ridges <strong>in</strong> the<br />

Northampton Complex at the northern end <strong>of</strong> the Perth Bas<strong>in</strong>, and <strong>in</strong> the Leeuw<strong>in</strong><br />

Complex on the western marg<strong>in</strong> <strong>of</strong> the Bunbury Trough.<br />

Basement lithologies were estimated for the Perth Bas<strong>in</strong> based on the known<br />

basement lithology <strong>of</strong> nearby wells, and the cont<strong>in</strong>uation <strong>of</strong> geophysical signatures<br />

(gravity and magnetics) from areas <strong>of</strong> known basement compositions. For some<br />

wells, especially those <strong>in</strong> areas <strong>of</strong> very deep sedimentary sections (>10 km), a<br />

determ<strong>in</strong>ation was not made due to the lack <strong>of</strong> <strong>in</strong>formation available to allow for a<br />

reasonable level <strong>of</strong> certa<strong>in</strong>ty <strong>in</strong> determ<strong>in</strong><strong>in</strong>g the lithologies. For all other wells <strong>in</strong> this<br />

study, however, basement lithology was estimated. Attachment C details <strong>in</strong>dividual<br />

lithology estimates for the 170 wells not previously studied, and Attachment D for the<br />

80 previously studied wells.<br />

While HDRPL has drawn on all available <strong>in</strong>formation, the exact nature <strong>of</strong> the<br />

basement <strong>of</strong> the Perth Bas<strong>in</strong> rema<strong>in</strong>s poorly constra<strong>in</strong>ed. Gravity data are <strong>of</strong> limited<br />

use for lithology determ<strong>in</strong>ation <strong>in</strong> much <strong>of</strong> the Perth Bas<strong>in</strong> ow<strong>in</strong>g to the great<br />

thickness <strong>of</strong> the post-Permian succession. Lithology estimates for basement were<br />

guided by basement lithologies <strong>in</strong>tersected <strong>in</strong> wells, and the assumption that a similar<br />

lithology may be expected with<strong>in</strong> a 10 km radius—the approximate size <strong>of</strong> a small<br />

pluton. Wells outside these areas are denoted as hav<strong>in</strong>g an “unknown” basement<br />

lithology, although it is probable that many <strong>of</strong> these “unknown” lithologies are pre-rift<br />

metasediments.<br />

6 Iasky R.P. 1994, Onshore northern Perth Bas<strong>in</strong> gravity project. In Geological Survey <strong>of</strong> <strong>Western</strong> <strong>Australia</strong>,<br />

1993-1994 Annual Review<br />

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