The dunitic mantle-crust transition zone in the Oman ophiolite: Residue of melt-rock interaction, cumulates from high-MgO melts, or both?
Author:
Publisher
Geological Society of America
Subject
Geology
Link
http://pubs.geoscienceworld.org/geology/article-pdf/41/1/67/3543670/67.pdf
Reference20 articles.
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2. Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry;Arai;Mineralogical Magazine,1992
3. Petrology of the gabbro-troctolite-peridotite complex from Hess Deep, equatorial Pacific: Implications for mantle-melt interaction within the oceanic lithosphere;Arai,1996
4. Trace element and isotopic characterization of mafic cumulates in a fossil mantle diapir (Oman ophiolite);Benoit;Chemical Geology,1996
5. Experimental determination of the diffusion coefficient for calcium in olivine between 900°C and 1500°C;Coogan;Geochimica et Cosmochimica Acta,2005
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4. EVIDENCE OF LITHOSPHERIC COOLING PRIOR TO MELT INFILTRATION HISTORY AT THE OMAN PALEO-SPREADING CENTRE (WADI TAYIN MASSIF);OFIOLITI;2023
5. Mantle property of Hegenshan ophiolite in Inner Mongolia: Constrains from element geochemistry and Re-Os isotopes of harzburgite;Acta Petrologica Sinica;2023
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