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Hydrologically-significant structures imaged by induced microseismicity in a 3km deep well in granite at Soultz (FR)
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, EAGE/SEG Research Workshop on Reservoir Rocks - Understanding reservoir rock and fluid property distributions - measurement, modelling and applications, Apr 2001, cp-55-00035
- ISBN: 978-94-6282-123-1
Abstract
During 1993, 25,000m³ of water was injected at a peak overpressure of 9 MPa into a 550 m section of granitic basement exposed below 2.75 km in well GPK1 at the EU's HDR site at Soultz (Rhinegraben) in France.