Hydrous aluminosilicate metasomatism in an intra-oceanic subduction zone: Implications from the Kurancali ultramafic-mafic cumulates within the Alpine Neotethys Ocean, Turkey

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2007-08-01

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Toksoy-Koksal, Fatma
Oberhaensli, Roland
Göncüoğlu, Mehmet Cemal

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https://hdl.handle.net/11511/52867

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Hydrous aluminosilicate metasomatism in an intra-oceanic subduction zone: Implications from the Kurancali (Turkey) ultramafic-mafic cumulates within the Alpine Neotethys Ocean Toksoy Köksal, Fatma; Göncüoğlu, Mehmet Cemal (2009-03-01) The Kurancali ultramafic-mafic cumulate body, an allochthonous ophiolitic sliver in central Anatolia, is characterized by the presence of abundant hydrous phases (phlogopite, pargasite) besides augitic diopside, plagioclase, and accessory amounts of rutile, sphene, apatite, zircon, and calcite. Based on modes of the essential minerals, the olivine-orthopyroxene-free cumulates are grouped as clinopyroxenite, hydrous clinopyroxenite, phlogopitite, hornblendite, layered gabbro, and diorite. Petrographical, min...
Hydrous aluminosilicate metasomatism in an intra oceanic subduction zone Implications from the Kurancali ultramafic mafic cumulates within the Alpine Neotethys Ocean Turkey Toksoy Köksal, Fatma; Oberhaenslı, Roland (2007-09-16)
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Citation Formats

F. Toksoy-Koksal, R. Oberhaensli, and M. C. Göncüoğlu, “Hydrous aluminosilicate metasomatism in an intra-oceanic subduction zone: Implications from the Kurancali ultramafic-mafic cumulates within the Alpine Neotethys Ocean, Turkey,” 2007, vol. 71, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/52867.