Record Details

Title Geothermal Reservoir Characterization in Crystalline Rock Using 3D Seismics (Schneeberg, Germany)
Authors Felix HLOUSEK, Olaf HELLWIG, Stefan BUSKE
Year 2015
Conference World Geothermal Congress
Keywords exploration, 3D seismic imaging, fault zones, enhanced geothermal systems
Abstract We present the results of a 3D seismic survey acquired near Schneeberg in the western Erzgebirge (Germany). The aim of the project is to use seismic exploration methods to image and to characterize a major fault zone in crystalline rock, which could be used as a natural heat exchanger at a target depth of about 5-6 km with expected temperatures between 160-180°C. The region itself is dominated by the NW-SE striking Gera-Jáchymov fault system. The main geological features in the survey area are well known from intensive mining activities down to a depth of about 2 km. The seismic investigations aimed at imaging the partly steeply dipping fault branches at greater depth, in particular a dominant NE dipping fault in the central part of the survey area with displacements up to 500 m. Beside this main structure, the Gera-Jáchymov fault zone consists of a couple of SW dipping conjugated faults. For the purpose of imaging and characterizing this fault zone, a high resolution 3D Vibroseis survey with more than 5300 source and approximately 8000 receiver locations was performed at the end of 2012 and covered an area of approximately 10 km x 13 km. The 3D survey was complemented by an additional wide-angle seismic survey using explosives along ten profile lines radially centered at the target area. Advanced processing and imaging methods have been applied to the data set. 3D Kirchhoff pre-stack depth migration delivered a clear image of various fault branches at depths of around 2-5 km. Furthermore, focusing migration methods (e.g. coherency migration) have been applied and have improved the image such that the 3D seismic result allows for a profound characterization of this potential geothermal reservoir in crystalline rock. Based on the 3D seismic image of the fault zone, potential drilling targets and paths are defined.
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