RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 18, ES3003, doi:10.2205/2018ES000622, 2018
Geol. age | $Q$ | $C_2$ | $V_2$ | $D_3-C_2$ (Autolithic breccia) | $D_3-C_2, \; V_2$ (Near-contact space) |
Number of samples | 10 | 31 | 54 | 13 | 32 |
Isotope ratio $^{234}$U/$^{238}$U, Bq/Bq |
0.94 0.54–1.13 |
0.92 0.37–1.34 |
0.94 0.46–1.20 |
1.00 0.80–1.14 |
1.24 0.85–3.57 |
Concentration of uranium, ppm |
7.66 0.63–46.13 |
1.32 0.41–5.94 |
2.11 0.32–10.73 |
0.67 0.33–1.07 |
1.66 0.40–5.93 |
Note. Above the bar – the average values, below the bar – the minimum and maximum values. |
Citation: Kiselev G. P., E. Yu. Yakovlev, S. V. Druzhinin, S. B. Zykov, V. M. Bykov, A. A. Ocheretenko (2018), Uranium even isotopes in kimberlites, enclosing and overburden rocks of the Zolotitskoye ore field (Arkhangelsk diamondiferous province), Russ. J. Earth Sci., 18, ES3003, doi:10.2205/2018ES000622.
Copyright 2018 by the Geophysical Center RAS.