Maturing processes of arc mantle deduced from ophiolites
Author:
Publisher
Japan Association of Mineralogical Sciences
Subject
Economic Geology,Geochemistry and Petrology
Reference162 articles.
1. Adachi, Y. and Miyashita, S. (2003): Geology and petrology of the plutonic complexes in the Wadi Fizh area: multiple magmatic events and segment structure in the northern Oman ophiolite. Geochem. Geophys. Geosys., 4, 8619, doi:10.1029/2001GC000272.
2. Ahmed, A.H. and Arai, S. (2002): Unexpectedly high-PGE chromitite from the deeper mantle section of the northern Oman ophiolite and its tectonic implications. Contrib. Mineral. Petrol., 143, 263-278.
3. Ahmed, A.H. and Arai, S. (2003): Platinum-group minerals in podiform chromitites of the Oman ophiolite. Can. Mineral., 41, 597-616.
4. Ahmed, A.H., Hanghøj, K., Kelemen, P.B., Hart, S.R. and Arai, S. (2006): Osmium isotope systematics of the Proterozoic and Phanerozoic ophiolitic chromitites: in situ ion probe analysis of primary Os-rich PGM. Earth Planet Sci. Lett., 245, 777-791.
5. Alabaster, T., Pearce, J.A. and Malpas, J. (1982): The volcanic stratigraphy and petrogenesis of the Oman ophiolite complex. Contrib. Mineral. Petrol., 81, 168-183.
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