Fig. 5From: Burial history and thermal maturity of Mesozoic rocks of the Dolomites, Northern ItalyPaleo water depth (PWD), sediment water interface temperature (SWIT) and heat flow (HF) over time. In the heatflow curve, the rifting of the continental crust (1) and the opening of the Ligurian-Piemontese Ocean (2) are highlightedBack to article page