RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES1001, doi:10.2205/2017ES000578, 2017


Table 2. Modal Composition (%) of Volcanic Rocks in the Udokan Range
Sample Phenocrysts Groundmass (Pl, Ol, Fe-Ti oxides Porosity Secondary minerals Facies
and Cpy microlites) (magnetite,
Pl Ol Cpy and volcanic glass ilmenite) $\quad$ Chl Id
506/6 - 13.7 - 81.4 - 4.9 - - Lava
511/3 25.0 38.5 15.8 20.7 - - - Lava
511/7 - 16.2- 64.8 19.0 - - - Lava
511/10 21.2 10.3- 68.5 - - - - Lava
511/13 19.2 22.2 - 51.6 - - 7.0 Lava
624/10 - 13.8 15.0 55.2 3.1 13.7 - - Lava
624/13 23.7 42.5 29.7 - 4.1 - - - Lava
628/9 11.3 19.8 33.1 - 9.7 - 26.1 - Lava
635/1 38.1 14.4 19.3 - 17.0 - 11.2 - Lava
636/3 8.7 - 7.1 52.6 16.1 - - - Lava
510/3 34.4 40.0 17.9 - 7.7 - - - Vent
625/4 8.8 35.2 39.0 - 17.0 - - - Vent
631/1 6.0 8.2 3.3 79.6 2.9 - - - Vent
510/5 39.5 27.822.9 - 9.8 - - - Explosion

      Powered by MathJax


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.


Generated from LaTeX source by ELXpaper, v.1.5 software package.