Characterization of the sources of thermal spring‐ and well water in Jordan by rare earth element and yttrium distribution and stable isotopes of H2O
- 10 April 2006
- journal article
- Published by Wiley in Acta Hydrochimica et Hydrobiologica
- Vol. 34 (1-2) , 101-116
- https://doi.org/10.1002/aheh.200500614
Abstract
No abstract availableKeywords
This publication has 43 references indexed in Scilit:
- Rare earth elements, yttrium and Pb isotope ratios in thermal spring and well waters of West Anatolia, Turkey: a hydrochemical study of their originChemical Geology, 2004
- Rare earths and yttrium hydrostratigraphy along the Lake Kinneret–Dead Sea–Arava transform fault, Israel and adjoining territoriesApplied Geochemistry, 2003
- Climatological signals of the paleogroundwater in JordanJournal of Hydrology, 2001
- Scavenging of dissolved yttrium and rare earths by precipitating iron oxyhydroxide: experimental evidence for Ce oxidation, Y-Ho fractionation, and lanthanide tetrad effectGeochimica et Cosmochimica Acta, 1999
- Geochemistry of low-temperature water–rock interaction: evidence from natural waters, andesite, and iron-oxyhydroxide precipitates at Nishiki-numa iron-spring, Hokkaido, JapanChemical Geology, 1998
- Determination of easily accessible metal fractions in rocks by batch leaching with acid cation-exchange resinChemical Geology, 1997
- Tetrad effect in lanthanide partitioning between calcium sulfate crystal and its saturated solutionChemical Geology, 1993
- Rare earth element fractionation in metamorphogenic hydrothermal calcite, magnesite and sideriteTschermaks Mineralogische und Petrographische Mitteilungen, 1992
- The stable isotope composition of Dead Sea watersEarth and Planetary Science Letters, 1984
- Isotopic analyses and hydrochemistry of the thermal springs along the eastern side of the Jordan Dead Sea—Wadi Araba Rift ValleyJournal of Hydrology, 1984