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Fig. 6
Influence of (a–b) radiogenic heating Qrad and (c–d) initial mantle temperature Tinit,mantle on (a, c) outgassing and (b, d) mantle depletion. The amount of outgassing of CO2 is denoted interms of partial pressure pCO_2. The cases 2–5 and the reference case are shown (Table 3).
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