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

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5<br />

2. Perth Bas<strong>in</strong> Geological Sett<strong>in</strong>g<br />

The Perth Bas<strong>in</strong> is a north-northwesterly oriented rift bas<strong>in</strong> extend<strong>in</strong>g approximately<br />

1000 km along the western marg<strong>in</strong> <strong>of</strong> south-western <strong>Australia</strong>, between latitudes<br />

27°00’S and 34°30’S. It is comprised <strong>of</strong> a series <strong>of</strong> sub-bas<strong>in</strong>s, troughs, shelves and<br />

ridges conta<strong>in</strong><strong>in</strong>g predom<strong>in</strong>antly Early Permian to Late Cretaceous sedimentary<br />

sequences up to 15 km thick (Freeman and Donaldson 2006 1 ). The Bas<strong>in</strong> extends<br />

from the Darl<strong>in</strong>g Fault <strong>in</strong> the east, which marks a discont<strong>in</strong>uity between the<br />

Phanerozoic sediments <strong>of</strong> the bas<strong>in</strong> and the Precambrian rocks <strong>of</strong> the adjacent<br />

Yilgarn Craton, to the edge <strong>of</strong> the cont<strong>in</strong>ental shelf to the west. To the north the bas<strong>in</strong><br />

grades <strong>in</strong>to the Southern Carnarvon Bas<strong>in</strong>. Precambrian rocks <strong>of</strong> the P<strong>in</strong>jarra Orogen<br />

underly the Perth Bas<strong>in</strong>. These crop out as fault bounded mid-bas<strong>in</strong> ridges <strong>in</strong> the<br />

Leeuw<strong>in</strong> and Northampton Complexes (Mory et al., 2005 2 ).<br />

The Perth Bas<strong>in</strong> is structurally complex and formed dur<strong>in</strong>g the separation <strong>of</strong> <strong>Australia</strong><br />

and Greater India <strong>in</strong> the Permian to Early Cretaceous. The structural architecture <strong>of</strong><br />

the Perth Bas<strong>in</strong> is the product <strong>of</strong> oblique rift<strong>in</strong>g dur<strong>in</strong>g the Permian, Late Triassic to<br />

Early Jurassic and Middle Jurassic to Early Cretaceous, superimposed over preexist<strong>in</strong>g<br />

basement terra<strong>in</strong>s (Mory and Iasky, 1996 3 ). Extension dur<strong>in</strong>g the Permian<br />

produced the series <strong>of</strong> deep, north-south trend<strong>in</strong>g rift bas<strong>in</strong>s (Bunbury Trough and<br />

Dandaragan Trough) along the western marg<strong>in</strong> <strong>of</strong> the Yilgarn Craton with syndepositional<br />

growth along the Darl<strong>in</strong>g Fault.<br />

Breakup was associated with widespread <strong>in</strong>version, erosion, strike-slip tectonics and<br />

volcanism, which significantly modified the structural architecture <strong>of</strong> the Perth Bas<strong>in</strong>.<br />

Major structural elements associated with breakup tectonism <strong>in</strong>clude an area <strong>of</strong><br />

1<br />

Freeman, M. J., And Donaldson, M. J., 2006, Geology <strong>of</strong> the southern Perth Bas<strong>in</strong> and Margaret River w<strong>in</strong>e<br />

district, southwestern <strong>Western</strong> <strong>Australia</strong> — a field guide: <strong>Western</strong> <strong>Australia</strong> Geological Survey, Record 2006/20<br />

2<br />

Mory, A. J., Haig, D. W., Mcloughl<strong>in</strong>, S., And Hock<strong>in</strong>g, R. M., 2005, Geology <strong>of</strong> the northern Perth Bas<strong>in</strong>,<br />

<strong>Western</strong> <strong>Australia</strong>— a field guide: <strong>Western</strong> <strong>Australia</strong> Geological<br />

Survey, Record 2005/9<br />

3<br />

Mory, A. J., And Iasky, R. P., 1996, Stratigraphy and structure <strong>of</strong> the onshore<br />

northern Perth Bas<strong>in</strong>, <strong>Western</strong><br />

<strong>Australia</strong>: <strong>Western</strong> <strong>Australia</strong> Geological Survey,<br />

Report 46<br />

www.hotdryrocks.com

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