The aqueous geochemistry of the rare earth elements and yttrium. Part 7. REE, Th and U contents in thermal springs associated with the Idaho batholith
- 30 September 1998
- journal article
- Published by Elsevier BV in Applied Geochemistry
- Vol. 13 (7), 861-884
- https://doi.org/10.1016/s0883-2927(98)00019-5
Abstract
No abstract availableKeywords
This publication has 92 references indexed in Scilit:
- The aquatic chemistry of rare earth elements in rivers and estuariesAquatic Geochemistry, 1995
- The aqueous geochemistry of the rare-earth elements and yttrium 4. Monazite solubility and REE mobility in exhalative massive sulfide-depositing environmentsChemical Geology, 1994
- Dispersion of U, Th, and REE by water-rock interaction around an intragranitic U-vein, Jalerys Mine, Morvan, FranceApplied Geochemistry, 1992
- A co‐precipitation technique for determining trace metal concentrations in iron‐rich saline solutionsEnvironmental Technology, 1990
- Determination of rare earth elements in hot spring and crater lake waters by epithermal neutron activation analysisJournal of Radioanalytical and Nuclear Chemistry, 1989
- Comparison of the solution chemistry of the actinides and lanthanidesJournal of the Less Common Metals, 1983
- Controls on source and depth of emplacement of granitic magmaGeology, 1981
- The generation of batholithsTectonophysics, 1973
- Areal Distribution and Geophysical Significance of Heat Generation in the Idaho Batholith and Adjacent Intrusions in Eastern Oregon and Western MontanaGSA Bulletin, 1973
- Thermodynamics of hydrothermal systems at elevated temperatures and pressuresAmerican Journal of Science, 1969