Garnet-Pyroxenite-Derived End-Member Magma Type in Kamchatka: Evidence from Composition of Olivine and Olivine-Hosted Melt Inclusions in Holocene Rocks of Kekuknaisky Volcano
2019 ◽
1975 ◽
Vol 27
(2)
◽
pp. 211-218
◽
Keyword(s):
Keyword(s):