Article ID Journal Published Year Pages File Type
4717161 Lithos 2010 16 Pages PDF
Abstract
Based on geochemical and isotopic characteristics this magmatic complex can be subdivided into 4 groups: a) gabbro, b) diorite to alkali granite (main body), c) syenite/monzonite and d) mafic dykes. Geochemical data and modelling results favour a typical subduction-related enriched lithospheric mantle and lower crustal source for the Demirköy Igneous Complex. Slab-derived fluids and crustal contamination also played a key role in the petrogenesis of this magmatic suite.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
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