Mobility of U-Th radionuclides connected with fault porosity: A case study of the Schauenburg Fault, Rhine Graben Shoulder, Germany

Physics and Chemistry of the Earth

Volumn 30, Issue 17-18 SPEC. ISS., 2005, Pages 1030-1037

  Marbach, Thierry ^a   Kober, Bernd ^b   Mangini, Augusto ^c   Warr, Laurence ^d   Schleicher, Anja ^a  

^a UNIVERSITY OF HEIDELBERG   (Germany)

^b Institute of Environmental Geochemistry   (Germany)

^c HEIDELBERG ACADEMY OF SCIENCES AND HUMANITIES   (Germany)

^d UMR 7063   (France)

Author keywords

Exchange model; Fault zone; Granite; Porosity; U Th radionuclides; Water rock interaction

Indexed keywords

COMPOSITION; GRANITE; LANDFORMS; MATHEMATICAL MODELS; MECHANICAL PERMEABILITY; PETROLOGY; POROSITY; RADIOISOTOPES; TECTONICS; THORIUM; URANIUM;

EXCHANGE MODEL; FAULT POROSITY; FAULT ZONE; WATER-ROCK INTERACTION;

STRUCTURAL GEOLOGY;

ELEMENT MOBILITY; FAULT ZONE; GRANITE; POROSITY; RADIONUCLIDE; THORIUM; URANIUM; WATER-ROCK INTERACTION;

CENTRAL EUROPE; EASTERN HEMISPHERE; EURASIA; EUROPE; RHINE GRABEN; WORLD;

EID: 28244461560     PISSN: 14747065     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pce.2005.02.001     Document Type: Article

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