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Victoria University Antarctic Research Expedition Science and Logistics Reports 1984-85: VUWAE 29

Figure 14. Model for the uplift history of the Transantarctic Mountains in the Miers Valley area based on observed apatite age variation versus elevation and the estimated depth to zero age. The dramatic change in uplift rate at 50 Myr from 15 Myr prior to this and 95 m/Myr after it has been interpreted using the uplift curve from Mt Doorly (Gleadow and Fitzgerald, in prep.)

Figure 14. Model for the uplift history of the Transantarctic Mountains in the Miers Valley area based on observed apatite age variation versus elevation and the estimated depth to zero age. The dramatic change in uplift rate at 50 Myr from 15 Myr prior to this and 95 m/Myr after it has been interpreted using the uplift curve from Mt Doorly (Gleadow and Fitzgerald, in prep.)

Figure 14. Model for the uplift history of the Transantarctic Mountains in the Miers Valley area based on observed apatite age variation versus elevation and the estimated depth to zero age. The dramatic change in uplift rate at 50 Myr from 15 Myr prior to this and 95 m/Myr after it has been interpreted using the uplift curve from Mt Doorly (Gleadow and Fitzgerald, in prep.)