The Sub-Crustal Magma Chamber Existence and Magma Ascent Rate for Klyuchevskoy Volcano (Kamchatka): Constrains from Ni Zonation in Olivine Phenocrysts

The Sub-Crustal Magma Chamber Existence and Magma Ascent Rate for Klyuchevskoy Volcano (Kamchatka): Constrains from Ni Zonation in Olivine Phenocrysts

Gavrilenko M.; Ozerov A.
xmlui.dri2xhtml.METS-1.0.item-citation: Gavrilenko M., Ozerov A. (2014) The Sub-Crustal Magma Chamber Existence and Magma Ascent Rate for Klyuchevskoy Volcano (Kamchatka): Constrains from Ni Zonation in Olivine Phenocrysts // Abstract V51A-4726 presented at 2014 Fall Meeting, AGU, San Francisco, Calif., 15-19 Dec..
Date: 2014

Show full item record

Files in this item

Files Size Format View
Gavrilenko-2014-AGU.pdf 528.6Kb application/pdf View/Open

This item appears in the following Collection(s)