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Chromites from the early Proterozoic Outokumpu-Jormua Ophiolite Belt: a comparison with chromites from Mesozoic ophiolites
Institution:1. Department of Earth Science, The University of Hong Kong, Hong Kong, China;2. State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;3. Department of Geological Engineering, Karadeniz Technical University, 61080 Trabzon, Turkey;4. State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing 100083, China;1. Department of Geology, Payame Noor University, P.O. Box 19395-3697, Tehran, Iran;2. Karadeniz Technical University, Department of Geological Engineering, 61080 Trabzon, Turkey;3. Karlsruhe Institute of Technology (KIT), Institute for Applied Geosciences, Kaiser Str. 12, 76131 Karlsruhe, Germany;4. Department of Geology, Shahid Bahonar University of Kerman, P.O. Box 133-76135, Kerman, Iran;5. Geoscience Faculty, Shahid Beheshti University of Tehran, Daneshju Blvd, P.O. Box: 1983963113, Tehran, Iran
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