Abstract
New magnetotelluric data suggest the Perth basin is as much as 14 km deep in the Dandaragan Trough, reducing to 2 km deep over the Beagle Ridge. The Darling Fault is associated with a conductivity anomaly and this suggests the fault may be a control on fluid flow in the basin. Conductors in the deep basin may be due to increased permeability or temperature and therefore may warrant further investigation as geothermal targets. Declaration
Original language | English |
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Qualification | Doctor of Philosophy |
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Award date | 13 Jul 2018 |
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Publication status | Unpublished - 2017 |