Читать книгу Isotopic Constraints on Earth System Processes - Группа авторов - Страница 45
2 Ca and K Isotope Fractionation by Diffusion in Molten Silicates: Large Concentration Gradients Are Not Required to Induce Large Diffusive Isotope Effects
ОглавлениеJames M. Watkins1, John N. Christensen2, Donald J. DePaolo2,3, and Frederick J. Ryerson4
1 Department of Earth Sciences, University of Oregon, Eugene, Oregon, USA
2 Earth and Environmental Science Area, Energy Geosciences Division, Lawrence Berkeley National Laboratory, Berkeley, California, USA
3 Department of Earth and Planetary Science, University of California, Berkeley, California, USA
4 Atmospheric, Earth, and Energy Division, Lawrence Livermore National Laboratory, Livermore, California, USA
