Western australia hosts several large sedimentary basins with the potential for hot sedimentary aquifers hsas. The heat generation is determined from the half life of the isotopes in the material as well as their decay types. With the uniform heat producing layer model and surface heat flow of 160 mw m 2 surface temperature of 22 c and the curie depth of 6 4 km below the ocean bottom the parameters in salem et al.
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