Deep origin of mantle peridotites from the Aladağ ophiolite, Turkey: Implication from trace element geochemistry of pyroxenes and mineralogy of ophiolitic diamonds
Author:
Funder
National Natural Science Foundation of China
Nanjing University
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geology
Reference123 articles.
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4. Conversion of low-pressure chromitites to ultrahigh-pressure chromitites by deep recycling: A good inference;Arai;Earth and Planetary Science Letters,2013
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1. Multistage evolution of the Aladağ mantle peridotites (S-Türkiye): Processes of partial melting and melt-peridotite interaction in Mid-Ocean Ridge and Subduction Zones;Geochemistry;2024-01
2. Mantle peridotites of ophiolites rarely preserve reliable records of paleo-oceanic lithospheric mantle;Earth-Science Reviews;2023-09
3. A record of metasomatism and crustal contamination of the Mediterranean lithosphere in chromitites of the Orhaneli Ophiolite Complex (NW Türkiye);Journal of Asian Earth Sciences;2022-09
4. Early Cretaceous subduction initiation of the proto-Caribbean plate: geochronological and geochemical evidence from gabbros of the Moa-Baracoa ophiolitic massif, Eastern Cuba;Lithos;2022-06
5. Ti-poor high-Al chromitites of the Moa-Baracoa ophiolitic massif (eastern Cuba) formed in a nascent forearc mantle;Ore Geology Reviews;2022-05
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