Abstract
The Menderes Massif in Turkey represents one of the largest metamorphic core complexes in the world. It is regarded as a section of lower continental crust exhumed along low-angle detachment faults in the Late Miocene during a period of extension that affected the entire Aegean province. Syn-extensional magmatic activity within the Menderes metamorphic core complex is predominantly felsic forming several plutons, whereas mantle-derived magmatism has not been known so far. Here, we present a detailed study of the petrology and geochemistry of previously unreported mafic to intermediate lamprophyres within the Menderes Massif and assess their role in the geodynamic evolution of the core complex.
| Original language | English |
|---|---|
| Article number | egac024 |
| Number of pages | 28 |
| Journal | Journal of Petrology |
| Volume | 63 |
| Issue number | 4 |
| Early online date | 16 Mar 2022 |
| DOIs | |
| Publication status | Published - 1 Apr 2022 |