Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data
The inversion of seismic data to infer rock microstructural properties and fluid flow patterns in the crust is a challenging issue. In this paper, we develop an effective medium model for estimating velocities in porous media including both pores and cracks and use it to derive the distribution of c...
Main Authors: | , , , , |
---|---|
Format: | Text |
Language: | English |
Published: |
2011
|
Subjects: | |
Online Access: | https://www.documentation.ird.fr/hor/fdi:010053140 |
id |
ftird:oai:ird.fr:fdi:010053140 |
---|---|
record_format |
openpolar |
spelling |
ftird:oai:ird.fr:fdi:010053140 2024-09-09T19:48:36+00:00 Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data Adelinet, M. /Dorbath, Catherine Le Ravalec, M. Fortin, J. Gueguen, Y. ISLANDE 2011 https://www.documentation.ird.fr/hor/fdi:010053140 EN eng https://www.documentation.ird.fr/hor/fdi:010053140 oai:ird.fr:fdi:010053140 Adelinet M., Dorbath Catherine, Le Ravalec M., Fortin J., Gueguen Y. Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data. 2011, 38, p. L03305 text 2011 ftird 2024-08-15T05:57:42Z The inversion of seismic data to infer rock microstructural properties and fluid flow patterns in the crust is a challenging issue. In this paper, we develop an effective medium model for estimating velocities in porous media including both pores and cracks and use it to derive the distribution of crack density beneath the Reykjanes Peninsula from accurate tomography data. Outside the active hydrothermal areas, crack density is shown to decrease with depth. There are two main reasons for this: the closure of cracks because of the increasing overburden and the secondary filling of cracks because of hydrothermal flows. However, crack density may locally increase with depth beneath the southwestern part of the Kleifarvatn lake. This is consistent with the presence of a deep reservoir with supercritical fluids under pressure, which may activate hydrofracturing processes. We recognize that capturing the link between seismic data and the physical properties of crust is very difficult. This study shows that a combination of mechanical concepts and effective medium theory contributes to improve our understanding of the phenomena occurring within the Icelandic crust. Citation: Adelinet, M., C. Dorbath, M. Le Ravalec, J. Fortin, and Y. Gueguen (2011), Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data, Geophys. Res. Lett., 38, L03305, doi:10.1029/2010GL046304. Text Islande IRD (Institute de recherche pour le développement): Horizon Reykjanes ENVELOPE(-22.250,-22.250,65.467,65.467) Kleifarvatn ENVELOPE(-21.979,-21.979,63.926,63.926) |
institution |
Open Polar |
collection |
IRD (Institute de recherche pour le développement): Horizon |
op_collection_id |
ftird |
language |
English |
description |
The inversion of seismic data to infer rock microstructural properties and fluid flow patterns in the crust is a challenging issue. In this paper, we develop an effective medium model for estimating velocities in porous media including both pores and cracks and use it to derive the distribution of crack density beneath the Reykjanes Peninsula from accurate tomography data. Outside the active hydrothermal areas, crack density is shown to decrease with depth. There are two main reasons for this: the closure of cracks because of the increasing overburden and the secondary filling of cracks because of hydrothermal flows. However, crack density may locally increase with depth beneath the southwestern part of the Kleifarvatn lake. This is consistent with the presence of a deep reservoir with supercritical fluids under pressure, which may activate hydrofracturing processes. We recognize that capturing the link between seismic data and the physical properties of crust is very difficult. This study shows that a combination of mechanical concepts and effective medium theory contributes to improve our understanding of the phenomena occurring within the Icelandic crust. Citation: Adelinet, M., C. Dorbath, M. Le Ravalec, J. Fortin, and Y. Gueguen (2011), Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data, Geophys. Res. Lett., 38, L03305, doi:10.1029/2010GL046304. |
format |
Text |
author |
Adelinet, M. /Dorbath, Catherine Le Ravalec, M. Fortin, J. Gueguen, Y. |
spellingShingle |
Adelinet, M. /Dorbath, Catherine Le Ravalec, M. Fortin, J. Gueguen, Y. Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data |
author_facet |
Adelinet, M. /Dorbath, Catherine Le Ravalec, M. Fortin, J. Gueguen, Y. |
author_sort |
Adelinet, M. |
title |
Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data |
title_short |
Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data |
title_full |
Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data |
title_fullStr |
Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data |
title_full_unstemmed |
Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data |
title_sort |
deriving microstructure and fluid state within the icelandic crust from the inversion of tomography data |
publishDate |
2011 |
url |
https://www.documentation.ird.fr/hor/fdi:010053140 |
op_coverage |
ISLANDE |
long_lat |
ENVELOPE(-22.250,-22.250,65.467,65.467) ENVELOPE(-21.979,-21.979,63.926,63.926) |
geographic |
Reykjanes Kleifarvatn |
geographic_facet |
Reykjanes Kleifarvatn |
genre |
Islande |
genre_facet |
Islande |
op_relation |
https://www.documentation.ird.fr/hor/fdi:010053140 oai:ird.fr:fdi:010053140 Adelinet M., Dorbath Catherine, Le Ravalec M., Fortin J., Gueguen Y. Deriving microstructure and fluid state within the Icelandic crust from the inversion of tomography data. 2011, 38, p. L03305 |
_version_ |
1809917934416429056 |