Spacial Distribution of Fluid Flow Paths in Fractured Granites - Application to EGS

J. Place; E. Le Garzic; Y. Géraud; M. Diraison and J. Sausse

doi:10.3997/2214-4609.20144177

Spacial Distribution of Fluid Flow Paths in Fractured Granites - Application to EGS
By J. Place, E. Le Garzic, Y. Géraud and M. Diraison and J. Sausse
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 1st EAGE Sustainable Earth Sciences (SES) Conference and Exhibition, Nov 2011, cp-268-00105
ISBN: 978-90-73834-22-4
DOI: https://doi.org/10.3997/2214-4609.20144177

Abstract

Two fractured variscan granites have been selected to investigate present and past percolated networks. The first case study is the geothermal site at Soultz-sous-Forêts (Rhine Graben). Borehole seismic (VSP) has been used to map in 3D some generally per

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2011-11-08

2024-04-26

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Spacial Distribution of Fluid Flow Paths in Fractured Granites - Application to EGS

Abstract

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The natural combination of full and image‐based waveform inversion

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Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

Fracture detection by Gaussian beam imaging of seismic data and image spectrum analysis

Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture