Abstract
The Styrian Basin (SB) is the westernmost basin within the Pannonian Basin Complex and is located in southeastern Austria, where the crustal thickness decreases from more than 40 km to less than 30 km. It can be divided into the West and the East Styrian Basin. The pre-Neogene basement includes Penninic and crystalline rocks overlain by Palaeozoic rocks. The age of the basin fill ranges from the early to late Miocene. Despite a long hydrocarbon exploration history, only a single sub-economic gas field has been discovered. The lack of commercial deposits is probably due to limited source rock quality and an unfavourable heat flow history. In contrast, a significant number of geothermal wells with a cumulative length of >54 km has been drilled in the East SB. The main geothermal reservoirs are fractured Palaeozoic carbonates and Miocene (Badenian) sandstones. Geothermal gradients in the SB are typically above 4 °C/100 m. The hottest geothermal well (Frutura GT1) produces water with a temperature of 125 °C (bottom hole temperature 138 °C) from a depth of ∼3.3 km. Utilization of geothermal energy in the SB includes balneology, district and greenhouse heating, production of medical salt, CO 2 and electricity.
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