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Mineral chemistry of ultramafic and mafic cumulates as an indicator of the arc-related origin of the Mersin ophiolite (southern Turkey)

✍ Scribed by Osman Parlak, Michel Delaloye, Ergüzer Bíngöl

Book ID
112751355
Publisher
Springer
Year
1996
Tongue
English
Weight
377 KB
Volume
85
Category
Article
ISSN
0016-7835

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Geochemical character and tectonic envir
Geochemical character and tectonic environment of ultramafic to mafic cumulate rocks from the Tekirova (Antalya) ophiolite (southern Turkey)
✍ Baǧci, Utku (author);Parlak, Osman (author);Höck, Volker (author) 📂 Article 📅 2006 🏛 John Wiley and Sons 🌐 English ⚖ 841 KB

## Abstract The Upper Cretaceous Tekirova (Antalya) ophiolite derived from the southern branch of the Neotethys is located at the southwestern part of the Antalya Complex along the Tauride belt in southern Turkey. It comprises harzburgitic tectonites, ultramafic to mafic cumulates, isotropic gabbro