Geochemical character and tectonic environment of ultramafic to mafic cumulate rocks from the Tekirova (Antalya) ophiolite (southern Turkey)

Author:

Bağci Utku,Parlak Osman,Höck Volker

Publisher

Wiley

Subject

Geology

Reference77 articles.

1. Petrology of mafic inclusions from Itinome-gata, Japan

2. The Petrology of Plutonic Blocks and Inclusions from the Lesser Antilles Island Arc

3. , , . 2002. Suprasubduction zone origin of the Antalya ophiolite (southern Turkey) deduced from mineral chemistry of the ultramafic-mafic cumulates. 1st International Symposium of the Faculty of Mines (İTÜ) on Earth Sciences and Engineering, 16–18 May 2002, İstanbul, Turkey, Abstracts; 140.

4. Whole-rock and mineral chemistry of cumulates from the Kızıldağ (Hatay) ophiolite (Turkey): clues for multiple magma generation during crustal accretion in the southern Neotethyan ocean

5. 1992. Petrology and geochemistry of the plutonic rocks of the Halmahera ophiolite, eastern Indonesia, an analogue of modern oceanic forearcs. In Ophiolites and Their Modern Oceanic Analogues, , (eds). Special Publication 60. Geological Society: London; 179–202.

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