RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 14, ES1001, doi:10.2205/2014ES000535, 2014
Grain number | Ti content, ppm | Temperature, ° C |
of zircons | ||
2 | 14.31 | 769 |
3 | 12.39 | 756 |
4 | 14.65 | 771 |
5 | 6.24 | 697 |
6 | 22.70 | 814 |
9 | 7.54 | 713 |
10 | 12.91 | 760 |
12 | 8.37 | 722 |
13 | 20.87 | 805 |
16 | 14.77 | 772 |
17 | 19.88 | 801 |
19 | 31.46 | 848 |
20 | 19.13 | 797 |
24 | 11.94 | 753 |
25 | 26.03 | 828 |
26 | 115.39 | 1007 |
27 | 16.44 | 782 |
30 | 5.98 | 694 |
32 | 22.02 | 811 |
33 | 13.12 | 761 |
35 | 1.72 | 604 |
37 | 4.25 | 667 |
38 | 10.50 | 741 |
39 | 13.45 | 763 |
40 | 12.25 | 755 |
41 | 27.26 | 833 |
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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