Iron isotopic fractionation and origin of chromitites in the paleo-Moho transition zone of the Kop ophiolite, NE Turkey

Lithos3.50
Volume: 268-271, Pages: 65 - 75
Published: Jan 1, 2017
Abstract
The paleo-Moho transition zone (MTZ) of the Kop ophiolite in NE Turkey is mainly composed of dunites, which are locally interlayered with chromitites and contain minor relics of harzburgites. Large Fe isotopic variations were observed for magnesiochromite (− 0.14 to 0.06‰) and olivine (− 0.12 to 0.14‰) from the MTZ rocks. In individual samples, magnesiochromite has lighter Fe isotopic compositions than olivine, which was probably caused by...
Paper Details
Title
Iron isotopic fractionation and origin of chromitites in the paleo-Moho transition zone of the Kop ophiolite, NE Turkey
Published Date
Jan 1, 2017
Journal
Volume
268-271
Pages
65 - 75
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