Titlebook: Hydrogeology of Crystalline Rocks; Ingrid Stober,Kurt Bucher Book 2000 Springer Science+Business Media Dordrecht 2000 Geoinformationssyste

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Ian Parsons,Martin R. Lee techniques will find this volume of tremendous benefit as they move towards new directions in the exciting and expanding field of biological aging. .978-1-62703-906-2978-1-59745-361-5Series ISSN 1064-3745 Series E-ISSN 1940-6029

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Ancient Microbial Activity in Crystalline Bedrock — Results from Stable Isotope Analyses of Fractureground bacteria have been successfully identified (e.g. Pedersen and Karlsson, 1995; Pedersen, this volume). However, sampling of groundwater in boreholes always involves a number of question-marks concerning representativity, undisturbed conditions and actual depth of the water and consequently also the microbes sampled.

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Book 2000ast years that highly mineralized wateris present in an interconnected fracture network of the basement.Thus, the upper part of the crust of the continents can be viewed asan aquifer and investigated with tools common in hydrogeology. .This book presents accounts on water-conducting features ofcryst

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0921-092X ring the past years that highly mineralized wateris present in an interconnected fracture network of the basement.Thus, the upper part of the crust of the continents can be viewed asan aquifer and investigated with tools common in hydrogeology. .This book presents accounts on water-conducting featur

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Alkali Feldspars as Microtextural Markers of Fluid Flowxtures can provide unique insights into paths of fluid flow and mass transfer through crystalline rocks from the nanometre to the kilometre scale. The main thermodynamic driving force for the microtextural changes is elastic strain energy associated with coherency in strain-controlled microperthitic

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Hydraulic Properties of the Upper Continental Crust: data from the Urach 3 geothermal well a general interpretation of the hydraulic properties of crystalline continental upper crust. The typical granitic and gneissic basement contains an interconnected fluid-filled fracture system and behaves hydraulically like a confined fractured aquifer. Thus standard hydraulic well-tests can be used

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