Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4717161 | Lithos | 2010 | 16 Pages |
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
Authors
Zekiye Karacık, Okan Tüysüz,