Vermiculitization of phlogopites within metagabbro, Central Turkey

Date

1999-09-09

Author

Toksoy Köksal, Fatma
İçöz, Serap
Göncüoğlu, M. Cemal

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https://hdl.handle.net/11511/82165

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Vermiculitization of phlogopite in Metagabbro, central Turkey Toksoy Köksal, Fatma; Göncüoğlu, Mehmet Cemal (2001-02-01) Dioctahedral vermiculite occurs in an isolated metagabbro klippe (Kurancali Metagabbro) that belongs to the Central Anatolian Ophiolites from central Turkey. Both the metagabbro and the structurally underlying high-grade metamorphic rocks are intruded by granitic rocks. The Kurancali Metagabbro is characterized by its well-developed compositional layering, and the presence of vermiculitized phlogopite rich layers. Petrographic and mineralogic studies show that the primary mineral phases in the host rock are...
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Citation Formats

F. Toksoy Köksal, S. İçöz, and M. C. Göncüoğlu, “Vermiculitization of phlogopites within metagabbro, Central Turkey,” 1999, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/82165.