Extended Data Figure 7: Shallow temperature gradient predicted by models at DFDP-1B.
From: Extreme hydrothermal conditions at an active plate-bounding fault
Note that the temperature gradient may be slightly over-estimated by the model, because local fault curvature is not accurately resolved by our model and the DFDP-1B location is placed slightly farther into the base of the hanging wall in the model than it is in reality.