3D model of fracture zones at Soultz-sous-Forêts based on geological data, image logs, induced microseismicity and vertical seismic profiles

This study presents a new deterministic 3D model of the fracture zones observed in the granitic reservoir of the Soultz European geothermal project. The major fracture zones encountered around 6 wells (4550, EPS1, GPK1, GPK2, GPK3 and GPK4) consist in 53 main structures that are located and characterized in terms of size and orientation: 39 fracture zones, 8 microseismic structures and 6 structures derived from vertical seismic profiles are represented in the 3D model using Discrete Fracture Network tools of the gOcad modelling platform (Paradigm™, Earth Decision™). This work illustrates the complexity of 3D fracture zone correlation and interpretation in crystalline rock masses characterized at meter scale (borehole) and at the reservoir scale (kilometer) thanks to geophysical imaging techniques.

[1]  Albert Genter,et al.  Permeability and alteration within the Soultz granite inferred from geophysical and flow log analysis. , 2006 .

[2]  A. Genter Géothermie roches chaudes sèches : le granite de Soultz-sous-Forêts (Bas-Rhin, France) : fracturation naturelle, altérations hydrothermales et interaction eau-roche , 1989 .

[3]  C. Castaing,et al.  Comparative analysis of direct (core) and indirect (borehole imaging tools) collection of fracture data in the Hot Dry Rock Soultz reservoir (France) , 1997 .

[4]  Philippe Renard,et al.  Three-dimensional geometric modeling of a faulted domain: the Soultz Horst example (Alsace, France) , 1994 .

[5]  A. Beauce,et al.  Seismic studies on the HDR site of Soultz-sous-Forêts (Alsace, France) , 1991 .

[6]  J. Pinault,et al.  Tracer testing of the geothermal heat exchanger at Soultz-sous-Forêts (France) between 2000 and 2005 , 2006 .

[7]  A. Genter,et al.  Analysis of macroscopic fractures in granite in the HDR geothermal well EPS-1, Soultz-sous-Foreˆts, France , 1996 .

[8]  Albert Genter,et al.  Seismic response of the fractured and faulted granite of Soultz-sous-Forêts (France) to 5 km deep massive water injections , 2009 .

[9]  Nicolas Cuenot,et al.  Analysis of the Microseismicity Induced by Fluid Injections at the EGS Site of Soultz-sous-Forêts (Alsace, France): Implications for the Characterization of the Geothermal Reservoir Properties , 2008 .

[10]  Chrystel Dezayes,et al.  Decoupling of deformation in the Upper Rhine Graben sediments. Seismic reflection and diffraction on 3-component Vertical Seismic Profiling (Soultz-sous-Forêts area) , 2009 .

[11]  Chrystel Dezayes,et al.  Deep-seated geology of the granite intrusions at the Soultz EGS site based on data from 5 km-deep boreholes , 2006 .

[12]  Chrystel Dezayes,et al.  Structure of the low permeable naturally fractured geothermal reservoir at Soultz , 2010 .

[13]  B. Valley The relation between natural fracturing and stress heterogeneities in deep-seated crystalline rocks at Soultz-sous-Forêts (France) , 2007 .

[14]  J. Mallet,et al.  3D Fracture Modeling Integrating Geomechanics and Geologic Data. , 2004 .

[15]  Albert Genter,et al.  Fracture analysis and reservoir characterization of the granitic basement in the HRD Soultz project (France) , 1995 .