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those which occur presently in regions of elevated geotherms By contrast, geophysical surveys and isotopic studies of mantle nodules suggest that the cratonic mantle is strong and cool and that the geotherm has been relatively low since the Archean (Section 1131) Some of the most compelling evidence of cool mantle lithosphere comes from thermobarometric studies of silicate inclusions in Archean diamonds, which suggest that temperatures at depths of 150 200 km during the Late Archean were similar to the present-day temperatures at those depths (Boyd et al, 1985; Richardson et al, 2001) Although geoscientists have not yet reconciled this apparent inconsistency, the relationship provides important boundary conditions for thermal models of Archean and Proterozoic tectonic processes.

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In addition to allowing estimates of ancient mantle geotherms, the evidence from mantle xenoliths indicates that the cool mantle roots beneath the cratons quickly reached their current thickness of 200 km during Archean times (Pearson et al, 2002; Carlson et al, 2005) This thickness is greater than that of old oceanic lithosphere but much thinner than it would be if the lithosphere simply had cooled from above by conduction since the Archean (Sleep, 2005) Progressive thickening by conductive cooling also can be ruled out because the mantle roots do not display an age progression with depth (James & Fouch, 2002; Pearson et al, 2002) Instead, the relatively small thickness and longterm preservation of the cratonic roots indicate that they must have been kept thin by convective heat transfer from the underlying mantle (Sleep, 2003).

03

Timing advance (km)

Once the cratonic roots stabilized, the heat supplied to the base of the lithosphere from the rest of the mantle must have been balanced by the heat that ows upward to the surface In this model, a chemically buoyant layer of lithosphere forms a highly resistant lid above the convecting mantle, allowing it to maintain nearly constant thickness over time These considerations illustrate how the formation and long-term survival of the cool mantle roots beneath the cratons has helped geoscientists constrain the mechanisms of heat transfer during Precambrian times Differences in the inferred mechanism of heat loss from the Earth s interior have resulted in contrasting views about the style of tectonics that may have operated during Precambrian times (eg Hargraves, 1986; Lowman et al, 2001; van Thienen et al, 2005) A conventional view suggests that an increased heat supply in.

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