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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2007-09-16

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Toksoy Köksal, Fatma
Oberhaenslı, Roland

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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-Koksal, Fatma; Oberhaensli, Roland; Göncüoğlu, Mehmet Cemal (2007-08-01)
Hydro-mechanical behavior of unsaturated specimens isotropically reconstituted from slurry and compacted specimens Ahmadi Naghadeh, Reza; Toker, Nabi Kartal; Department of Civil Engineering (2016) Response of unsaturated soils constitutes an important consideration for many problems in geotechnical engineering. The main objective of this study is to understand coupling hydro-mechanical behavior of the unsaturated reconstituted specimens from slurry and moist-tamped compacted specimen, and to develop practical and cost-effective testing equipment and procedure. The innovations that will be put forth by this study will make the unsaturated soil mechanics more accessible and appealing to those practical...
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Citation Formats

F. Toksoy Köksal and R. Oberhaenslı, “Hydrous aluminosilicate metasomatism in an intra oceanic subduction zone Implications from the Kurancali ultramafic mafic cumulates within the Alpine Neotethys Ocean Turkey,” 2007, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/85813.