Dunites in the mantle section of the Oman ophiolite – The boninite connection

Author:

Rollinson Hugh

Funder

Sultan Qaboos University

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference52 articles.

1. Spinel-free dunites as a proxy to komatiitic melt activity in the mantle;Abbou Kabir;Lithos,2015

2. Origin of spinel-free dunite veins from northern Oman ophiolite: possible involvement of a komatiitic melt;Abbou-Kabir;Journal of Mineralogical and Petrological Sciences,2011

3. The dunitic mantle-crust transition zone in the Oman ophiolite: residue of melt-rock interaction, cumulates from high-MgO melts or both?;Abily;Geology,2012

4. High pressure experimental calibration of the olivine-orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantle;Ballhaus;Contributions to Mineralogy and Petrology,1991

5. The petrogenesis of peridotitic komatiites: evidence from high pressure melting experiments;Bickle;Earth and Planetary Science Letters,1997

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