doi.org/10.1016/j.jafrearsci.2019.103667
Original paper

Multi-stage evolution of forearc mantle peridotites of Kağızman Ophiolite (Ağrı-eastern Anatolia)

Tijen Üner
2
Journal of African Earth Sciences2.30
Volume: 161, Pages: 103667 - 103667
Published: Jan 1, 2020
Abstract
The Kağızman Ophiolite, constituting the easternmost part of Tethys ophiolites in Anatolia, is located on the İzmir-Ankara-Erzincan ophiolitic belt. Ophiolitic rocks include a range of mantle peridotites, gabbros, pillow basalts and isolated sheeted dykes. The studied mantle peridotites are investigated with regard to geochemical and petrographical characteristics. MgO content of peridotites varies from 41.24 to 45.63 wt % while that of Al2O3 is...
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Paper Details
Title
Multi-stage evolution of forearc mantle peridotites of Kağızman Ophiolite (Ağrı-eastern Anatolia)
DOI
doi.org/10.1016/j.jafrearsci.2019.103667
Published Date
Jan 1, 2020
Journal
Journal of African Earth Sciences
Volume
161
Pages
103667 - 103667
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