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Title

Rare earth element concentrations in mafisc from the Kizil Dag ophiolite (Hatay, Turkey)

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Published in İzdar, Erol & Nakoman, Eran. Sixth Colloquium on Geology of the Aegean Region. İzmir - 19th September-4th October 1977 - İzmir: Dokuz Eylül University. 1985, p. 99-104
Collection Piri Reis international contribution series; 2
Abstract Abundances of rare earth elements (REE) from the mafic sequence of the Kizil Dagh-Hatay ophiolite have been measured by neutron activation technique for short lived isotopes. The reisults for twelve samples from the gabbroic part show a general REE pattern with a depletion in the light REE (LREE) indicating that these rocks were derived from a uniform LREE depleted asthenosphere source (SCHILLING, 1975) at a spreading zone. The REE abundances vary by a factor of 6 to 10 between the cumulate gabbros from the ultramafic - mafic transition zone and the high level microgabbros from screens in the dyke complex.
Note 2nd ed. ; texte en anglais avec résumés en turc et en anglais
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Swiss National Science Foundation: 2.322-076
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DELALOYE, Michel et al. Rare earth element concentrations in mafisc from the Kizil Dag ophiolite (Hatay, Turkey). In: İzdar, Erol & Nakoman, Eran (Ed.). Sixth Colloquium on Geology of the Aegean Region. İzmir. İzmir : Dokuz Eylül University, 1985. p. 99-104. (Piri Reis international contribution series; 2) https://archive-ouverte.unige.ch/unige:143468

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