Carbon and nitrogen isotopes and mineral inclusions in diamonds from chromitites of the Mirdita ophiolite (Albania) demonstrate recycling of oceanic crust into the mantle

2019/01/03 by Weiwei Wu, Jingsui Yang, Richard Wirth +4 · 1 citation
Earth and Planetary Sciences · #Geological and Geochemical Analysis #High-pressure geophysics and materials #earthquake and tectonic studies

paper · doi:10.2138/am-2019-6751

Abstract

Author: Wu, Weiwei et al.; Genre: Journal Article; Finally published : 2019; Title: Carbon and nitrogen isotopes and mineral inclusions in diamonds from chromitites of the Mirdita ophiolite (Albania) demonstrate recycling of oceanic crust into the mantle

Cited by

• Oceanic and super-deep continental diamonds share a transition zone origin and mantle plume transportation. [europepmc]

Related

• Recurrent Local Melting of Metasomatised Lithospheric Mantle in Response to Continental Rifting: Constraints from Basanites and Nephelinites/Melilitites from SE Germany
• Imperfections in natural diamond: the key to understanding diamond genesis and the mantle
• The Petrogenesis of Some Migmatites and Granites (Central Damara Orogen, Namibia): Evidence for Disequilibrium Melting, Wall-Rock Contamination and Crystal Fractionation
• A review of feldspar alteration and its geological significance in sedimentary basins: From shallow aquifers to deep hydrocarbon reservoirs
• Sublithospheric and lithospheric diamonds from the Candle Lake C29/30 kimberlite, Sask Craton