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| Titel |
Mantle Peridotites from the Mersin Ophiolite (S-Turkey): implications for effects of melting and subsequent melt interaction on whole-rock and mineral compositions |
| VerfasserIn |
Samet Saka, İbrahim Uysal, Recep Melih Akmaz, Melanie Kaliwoda, Utku Bagci |
| Konferenz |
EGU General Assembly 2014
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| Medientyp |
Artikel
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| Sprache |
Englisch
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| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 16 (2014) |
| Datensatznummer |
250086739
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| Publikation (Nr.) |
 EGU/EGU2014-660.pdf |
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| Zusammenfassung |
| Mersin ophiolite, from the middle Tauride, southern Turkey, is represented by mantle unit and
overlying crustal sections composed of ultramafic to mafic cumulates and basalts. Mantle
peridotites are composed mainly of harzburgite and dunite. They are variously depleted,
compared to the primitive mantle, and are characterized by very low TiO2 ( |
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