A review of the nature of magmatism in central Anatolia during the Mesozoic post-collisional period

Date

2001-08-01

Author

Duzgoren-Aydin, NS
Malpas, J
Göncüoğlu, Mehmet Cemal
Erler, A

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Magmatism in central Anatolia is characterized by petrographically and chemically distinct granitic and syenitic rocks. The granitic magmatism comprises C-type (crustal-derived) and H-type (hybrid) monzogranites and monzonites. Garnet-bearing C-type leucogranites represent the oldest magmatic phase, but younger hornblende +/- biotite +/- K-feldspar H-type plutons dominate the geology of the Central Anatolian Crystalline Complex (CACC). These typically include mafic microgranular enclaves. The granitic magmatism predates syenitic intrusions, among which quartz-bearing syenites were emplaced prior to feldspathoid-bearing ones.

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URI

https://hdl.handle.net/11511/30127

Journal

INTERNATIONAL GEOLOGY REVIEW

DOI

https://doi.org/10.1080/00206810109465042

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Graduate School of Natural and Applied Sciences, Article

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Citation Formats

N. Duzgoren-Aydin, J. Malpas, M. C. Göncüoğlu, and A. Erler, “A review of the nature of magmatism in central Anatolia during the Mesozoic post-collisional period,” INTERNATIONAL GEOLOGY REVIEW, pp. 695–710, 2001, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/30127.