Abstract
Research Article| January 01, 2003 U-Th-Ra Fractionation During Weathering and River Transport F. Chabaux; F. Chabaux Centre de Géochimie de la Surface (CNRS/ULP), Ecole et Observatoire des Sciences de la Terre, 1 rue Blessig 67084 Strasbourg Cedex, France Search for other works by this author on: GSW Google Scholar J. Riotte; J. Riotte Centre de Géochimie de la Surface (CNRS/ULP), Ecole et Observatoire des Sciences de la Terre, 1 rue Blessig 67084 Strasbourg Cedex, France Search for other works by this author on: GSW Google Scholar O. Dequincey O. Dequincey Centre de Géochimie de la Surface (CNRS/ULP), Ecole et Observatoire des Sciences de la Terre, 1 rue Blessig 67084 Strasbourg Cedex, France Search for other works by this author on: GSW Google Scholar Author and Article Information F. Chabaux Centre de Géochimie de la Surface (CNRS/ULP), Ecole et Observatoire des Sciences de la Terre, 1 rue Blessig 67084 Strasbourg Cedex, France J. Riotte Centre de Géochimie de la Surface (CNRS/ULP), Ecole et Observatoire des Sciences de la Terre, 1 rue Blessig 67084 Strasbourg Cedex, France O. Dequincey Centre de Géochimie de la Surface (CNRS/ULP), Ecole et Observatoire des Sciences de la Terre, 1 rue Blessig 67084 Strasbourg Cedex, France Publisher: Mineralogical Society of America First Online: 03 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2003) 52 (1): 533–576. https://doi.org/10.2113/0520533 Article history First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation F. Chabaux, J. Riotte, O. Dequincey; U-Th-Ra Fractionation During Weathering and River Transport. Reviews in Mineralogy and Geochemistry 2003;; 52 (1): 533–576. doi: https://doi.org/10.2113/0520533 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search The potential of radioactive disequilibria as tracers and chronometers of weathering processes has been recognised since the 1960’s (e.g., Rosholt et al. 1966; Hansen and Stout 1968). This interest results from the dual property of the nuclides of the U and Th radioactive series (1) to be fractionated during water-rock interactions and (2) to have radioactive periods of the same order of magnitude as the time constants of many weathering processes and chemical transfers to ground and river waters. Therefore, the study of radioactive disequilibria in surface environments should help to bring information about the nature, the intensity... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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