Fig. 2From: A novel workflow for geothermal exploration: 3D seismic interpretation of biohermal buildups (Upper Jurassic, Molasse Basin, Germany)Detail view of the Late Jurassic showing the northern edge of the Tethys ocean, the opening of the Central Atlantic Ocean, and the surrounding landmasses (Blakey 2015). During the Upper Jurassic, up to 600-m-thick carbonates were deposited in South Germany, with a simplified North-East/South-West proximal–distal trendBack to article page