Fig. 6
From: Burial history and thermal maturity of Mesozoic rocks of the Dolomites, Northern Italy
Results of sensitivity analyses of the Grödnertal model. A second model in the Frötschbach area shows same results. Simulated are the predefined HF curve (Fig. 5) with changing eroded thickness (a), changing eroded thickness at a fixed HF of 65 mW/m2, held constantly over time (b) and changing constant HFs at a constant eroded thickness of 1200 m (c). The lines in the plot represent the calculated VR. The VR data used for calibration is indicated by crosses (+). Depth is referring to sea level