Fig. 7From: Burial history and thermal maturity of Mesozoic rocks of the Dolomites, Northern ItalyBurial plot with temperature history of the Gardena Valley model (a) and the vitrinite reflectance evolution of Bellerophon and Buchenstein Fm. Simulated with the predefined HF curve and the best fitting eroded thickness of 1800 m (see Fig. 6a)Back to article page