RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES1001, doi:10.2205/2017ES000578, 2017
| Sample | Rock | Sampling site | K, % | $^{40}$Ar, $10^{-8}$ cm$^3$/g | $^{40}$Ar, rad | Age, Ma | Reference |
| 511/10 | Py-Ol | L. Burichi | 2.65 | 40 | $2.5 \pm 0.5$ | M. M. Arakelyants | |
| basalt | (IGEM), 1970 | ||||||
| 625/1 | Ol | L. Kuas | 1.67 | 60 | $5.0 \pm 1.0$ | same, 1970 | |
| basalt | |||||||
| 624 | Ol | L. Kuas | 2.04 | 60 | $1.8 \pm 0.15 $ | same, 2000 | |
| basalt | |||||||
| 625/1 | Ol | same place | 1.62 | 50 | 40 | $ 6.0 \pm 1.5 $ | [Drubetskoi and Grachev, 1987] |
| basalt | |||||||
| 625/3 m | Ol | same place | 1.80 | 13 | 4 | $3.0 \pm 1.5 $ | same |
| basalt | |||||||
| 625/4 | Ol | same place | 1.19 | 160 | 13 | $ 5.5 \pm 1.0 $ | same |
| basalt |
Citation: Grachev A. F. (2017), The nature of Late Cenozoic volcanism in the Udokan Range, northwestern segment of the Baikal Rift Zone, Russ. J. Earth Sci., 17, ES1001, doi:10.2205/2017ES000578.
Copyright 2017 by the Geophysical Center RAS.