Determination of fluid-flow zones in a geothermal sandstone reservoir using thermal conductivity and temperature logs-Reference-Cited by-同舟云学术

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Determination of fluid-flow zones in a geothermal sandstone reservoir using thermal conductivity and temperature logs

Published:2013-04 Issue: Volume:46 Page:32-41
ISSN:0375-6505
Container-title:Geothermics
language:en
Short-container-title:Geothermics

Author:

Haffen Sébastien,Geraud Yves,Diraison Marc,Dezayes Chrystel

Publisher

Elsevier BV

Subject

Geology,Geotechnical Engineering and Engineering Geology,Renewable Energy, Sustainability and the Environment

Reference44 articles.

1. Water–rock interaction processes in the Triassic sandstone and the granitic basement of the Rhine Graben: Geochemical investigation of a geothermal reservoir;Aquilina;Geochimica et Cosmochimica Acta,1997

2. Fluid flow along potentially active faults in crystalline rock;Barton;Geology,1995

3. Thermal anomalies indicate preferential flow along faults in unconsolidated sedimentary aquifers;Bense;Geophysical Research Letters,2008

4. Braided rivers within an arid alluvial plain (example from the Lower Triassic, western German Basin): recognition criteria and expression of stratigraphic cycles;Bourquin;Sedimentology,2009

5. Crustal-scale structure of the southern Rhine Graben from ECORS-DEKORP seismic-reflection data;Brun;Geology,1991

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