TY  - JOUR
ID  - epos1858
UR  - http://doi.org/10.1016/j.crte.2010.02.002
IS  - 7-8
A1  - Géraud, Yves
A1  - Rosener, Michel
A1  - Surma, Fabrice
A1  - Place, Joachim
A1  - Le Garzic, Édouard
A1  - Diraison, Marc
N2  - In EGS projects, fault zones are considered as the structures controlling deep flow at the reservoir scale. Using a large set of petrophysical properties (porosity, density, permeability, thermal conductivity [TC]) measured on cores collected along the EPS-1 borehole, a model of fault zone is proposed to describe them. A fault zone is a complex structure, showing different parts with different kinds of deformations and/or materials that could explain chemical and physical processes observed during fluid-rock interactions. The different parts composing the fault zone are: (1) the fault core or gauge zone; (2) the damage zone; (3) and the protolith. They are usually heterogeneous and show different physical properties. The damage zone is a potential high permeability channel and could become the main pathway for fluids if secondary minerals seal the fault core. Porosity is the lowest within the protolith, between 0.5 and 1%, but can go up to 15% in the fault zone. Permeability ranges from 10?20 m2 in the fresh granite to, at least, 10?15 m2 in the fault core, and TC ranges from 2.5 W K?1m?1 to 3.7 W K?1m?1. Finally, variations in specific surface are set over two orders of magnitude. If the lowest values usually characterize the fresh granite far from fault zones, physical properties could show variations spread over their whole respective ranges within these fault zones.
VL  - 342
TI  - Physical properties of fault zones within a granite body: Example of the Soultz-sous-Forêts geothermal site
AV  - none
EP  - 574
Y1  - 2010///
PB  - Elsevier
JF  - Comptes Rendus Geoscience
KW  - Granite; Fault zone; Porosity; Permeability; Thermal conductivity
SN  - 1631-0713
SP  - 566
ER  -