Fig. 5: Plume attributes with depth during ridge capture and de-anchoring. | Nature Communications

Fig. 5: Plume attributes with depth during ridge capture and de-anchoring.

From: Spreading ridge migration enabled by plume-ridge de-anchoring

Fig. 5

The key variables used to calculate the plume buoyancy flux (excess temperature, plume area, upwelling velocity) are plotted with depth for ridge capture (ad) and de-anchoring (eh) in two separate plume–ridge interactions (note the x-axes have different scales). These correspond to the plume–ridge interactions documented in Figs. 2 and 3. The evolution of each variable is captured by a unique line colour representing the simulation time from 0 to 100 Myr in 20 Myr increments.

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