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
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Geochemistry and tectonic significance of augen gneisses from the southern Menderes Massif (West Turkey) | ||
| Journal | Geological Magazine | ||
| Authors | Bozkurt, E. | Author | |
| Winchester, J. A. | Author | ||
| Park, R. G. | Author | ||
| Year | 1995 (May) | Volume | 132 |
| Page(s) | 287-301 | Issue | 3 |
| Publisher | Cambridge University Press (CUP) | ||
| DOI | doi:10.1017/s0016756800013613Search in ResearchGate | ||
| Mindat Ref. ID | 256592 | Long-form Identifier | mindat:1:5:256592:1 |
| GUID | b1e781ae-b69e-439e-b259-c166407c85c3 | ||
| 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 | ||
| 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 | ||
| In | (1995, May) Geological Magazine Vol. 132 (3) Cambridge University Press (CUP) | ||
| 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. | ||
References Listed
These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.
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| Not Yet Imported: - book : 10.1007/978-94-017-3373-1 If you would like this item imported into the Digital Library, please contact us quoting Book ID 9780412534102 | |
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