Figure 13 | Scientific Reports

Figure 13

From: Giant paleo-seafloor craters and mass wasting associated with magma-induced uplift of the upper crust

Figure 13

1D uplift cross plots for wells (a) 6403/6-1 (b) 6403/10-1 (c) 6404/11-1 and (d) 6302/6-1. Only well 6403/6-1 shows evidence of uplift and about 400 m to 700 m ± 200 m net erosion within the Springar Formation. Above the Springar Formation, about 750 m to 1000 m uplift is recorded within the Tare Formation. The first three wellbores are in areas where several magmatic sills have been interpreted while 6302/6-1 is outside the study area and not affected magmatic intrusions. N.B: The red circles highlight uplift at Springar, Tang and Kai levels.

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