| Reference Type | Journal (article/letter/editorial) |
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| Title | Geochemistry and tectonic significance of augen gneisses from the southern Menderes Massif (West Turkey) |
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| Journal | Geological Magazine |
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| Authors | Bozkurt, E. | Author |
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| Winchester, J. A. | Author |
| Park, R. G. | Author |
| Year | 1995 (May) | Volume | 132 |
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| Issue | 3 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800013613Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 256592 | Long-form Identifier | mindat:1:5:256592:1 |
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| GUID | 0 |
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| Full Reference | Bozkurt, E., Winchester, J. A., Park, R. G. (1995) Geochemistry and tectonic significance of augen gneisses from the southern Menderes Massif (West Turkey) Geological Magazine, 132 (3) 287-301 doi:10.1017/s0016756800013613 |
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| Plain Text | Bozkurt, E., Winchester, J. A., Park, R. G. (1995) Geochemistry and tectonic significance of augen gneisses from the southern Menderes Massif (West Turkey) Geological Magazine, 132 (3) 287-301 doi:10.1017/s0016756800013613 |
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| In | (1995, May) Geological Magazine Vol. 132 (3) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractThe protoliths of mylonitized augen gneisses exposed in the southern sector of the Menderes Massif (West Turkey) are calc-alkaline, peraluminous, S-type, late- to post-tectonic tourmaline- and garnet-bearing, two-mica leucogranites. They cut and post-date the fabrics of the ‘main Menderes metamorphism’ which took place between the early Eocene and early Oligocene and intrude metamorphic basement rocks comprising the so-called ‘Palaeozoic schist envelope’ of the massif. They are themselves cut by an extensive network of tourmaline-rich dykes. Chemical, mineralogical, isotopic and field relations suggest that the granitic protolith crystallized from a boron-rich, water-saturated melt, derived from partial melting of metagreywacke in the lower crust during peak Barrovian-type metamorphism. The protolith was probably emplaced during lateorogenic extensional collapse of the thickened crust in west Turkey during late Oligocene time. |
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