Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9527011 | Tectonophysics | 2005 | 9 Pages |
Abstract
Various disequilibrium features in alkali basalt of Zlot reflect complex convection effects and recharge, most probably in a shallow magma chamber. Major and trace elements data indicate that alkali basalts of Zlot originated from magmas deriving from metasomatized mantle wedge above a subducting and dehydrating plate. However the investigated rocks did not originate from primary magmas, but from a magma which has undergone considerable fractional crystallization.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Dragan MilovanoviÄ, Stevan Karamata, Miodrag BanjeÅ¡eviÄ,