(Table 1) Chemical composition of Middle Cenozoic magmatic rocks from the Schmidt Peninsula, North Sakhalin

Middle Cenozoic evolution of magmatism in the Schmidt Peninsula between 37 and 25 Ma began with eruptions of subalkaline and moderately alkaline andesite, latite, trachyandesite, and trachyrhyolite lavas and ended with subvolcanic intrusions of highly alkaline strongly undersaturated essexites. Acco...

Full description

Bibliographic Details
Main Authors: Rasskazov, S V, Simanenko, V P, Malinovsky, A I, Yasnygina, T A
Format: Dataset
Language:English
Published: PANGAEA 2007
Subjects:
FeO
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.745644
https://doi.org/10.1594/PANGAEA.745644