1. Internal thermal anomalies in
sedimentary basins caused by salt structures
Ben Norden
Salt structures like salt pillows and salt diapirs are quite common in sedimentary basins
Observable features: thermal anomalies
The thermal conductivity of rock salt is a factor of 2-3 higher than that of the typical surrounding rocks
Zones of special interests for the geothermal exploration?

2. Internal thermal anomalies in
sedimentary basins caused by salt structures
The knowledge of the salt structure geometry and the thermal properties of the involved rocks play a decisive role in the evaluation of a specific site.
On the poster:
Thermal modelling of salt structures of the Northeast German basin using 1-D, 2-D, and 3-D models.
Heat-flow density
[mW/m²]
Salt
Depth [m]