A.V.
Koloskov
State
Institute of Volcanic Geology and Geochemistry Far Eastern
Division, Russian Academy of Sciences.
Petropavlovsk-Kamchatsky,
683006. Piip boul.9
Geochemical and isotopic features coexisting arc-related and
intraplatelike types of volcanite’s in different regions of Kamchatka
were studied. These materials have been compared with data on
basalts, which have differ deeps origin. The comparison suggest
that the arc-related basalts peculiarities (Ta-Nb minimum and
K and Sr maximums) are appeared et the depth level of spinel
lherzolite – ol-pl peridotites transition. It is assumed that
both arc-related and intraplatelike volcanic rocks were derived
from single evolving mantle source.