RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 14, ES1001, doi:10.2205/2014ES000535, 2014
Element | Analytical | Analyzer | Modes of counter | Exposure | Standards | Detection limit, ppm |
line | crystals | operation | time, s | |||
Si | Ka | TAP | dif | 10 | Zircon | - |
P | Ka | TAP | dif | 90 | Apatite | 105 |
Fe | Ka | LIF | int | 100 | Andradite | 90 |
Zr | La | PET | int | 10 | Zircon | - |
Hf | Ma | TAP | dif | 100 | HfO$_2$ | 85 |
Y | La | TAP | dif | 90 | Y$_2$O$_3$ | 80 |
U | Ma | PET | int | 120 | UO$_2$ | 75 |
Th | Ma | PET | dif | 120 | ThO$_2$ | 70 |
Citation: Grachev A. F., S. E. Borisovsky, T. F. Zinger (2014), Morphology and geochemistry of zircon in bentonite ash at the Paleocene-Eocene boundary in the Anthering Formation, Eastern Alps, Austria, Russ. J. Earth Sci., 14, ES1001, doi:10.2205/2014ES000535.
Copyright 2014 by the Geophysical Center RAS.
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