Sie haben gesucht nach VerfasserIn: 'Legarzic, Edouard', in der Datenbank: Bibliothekskatalog.
Anzahl der Treffer: 8
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Structural analysis of an outcropping granite (Proterozoic basement of Yémen): faults and fractures distributions and scaling properties.
Le Garzic, Edouard; de L'Hamaide, Thibaut; Diraison, Marc; Geraud, Yves; de Urreiztieta, Marc; Hauville, Benoit; Champanhet, Jean-Michel
In: GRA - Volume 12
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2010
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| 2 |
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Investigation of fluid flow paths within granitic batholiths: the Soultz-sous-Forêts ‘Enhanced Geothermal System' and the Catalan Coastal Ranges examples
Place, Joachim; Geraud, Yves; Diraison, Marc; Le Garzic, Edouard; Sausse, Judith
In: GRA - Volume 12
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2010
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| 3 |
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Petrophysical properties of fault zones in granite body, implication for deep geothermal reservoir behaviour.
Geraud, Yves; Place, Joachim; Le Garzic, Edouard; Diraison, Marc; Staněk, Martin
In: GRA - Volume 13
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2011
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| 4 |
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Scaling and geometric properties of extensional fracture systems in the Proterozoic basement of Yemen
Le Garzic, Edouard; Geraud, Yves; Diraison, Marc
In: GRA - Volume 13
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2011
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| 5 |
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Multiscale analysis of the fracture pattern in granite, example of Tamariu's granite, Catalunya.
Bertrand, L.; LeGarzic, E.; Géraud, Y.; Diraison, M.
In: GRA - Volume 14
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2012
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| 6 |
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Use of markers of paleo-circulations to characterize the porous network of fractured granite.
Bertrand, L.; LeGarzic, E.; Géraud, Y.; Diraison, M.
In: GRA - Volume 14
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2012
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| 7 |
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Fractured crystalline reservoir: a power law over 8 orders of magnitude on length distribution but a size control on the connectivity. A field analog analysis: Tamariu's granite (Catalonian costal ranges).
Bertrand, Lionel; Legarzic, Edouard; Geraud, Yves; Diraison, Marc
In: GRA - Volume 15
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2013
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| 8 |
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Fractured reservoir analogs: case study of paelocirculation markers on Tamariu's Granite.
Bertrand, Lionel; Legarzic, Edouard; Geraud, Yves; Diraison, Marc
In: GRA - Volume 15
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2013
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Sie haben gesucht nach VerfasserIn: 'Legarzic, Edouard', in der Datenbank: Bibliothekskatalog.
Anzahl der Treffer: 8
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