View of Peridotitic diamond formation at Panda (Slave craton, Canada) from paleo-subduction wedge- or mantle-derived fluids ? The bearing of stable isotope data (15N/14N, 33S/32S, 34S/32S, /12C)

Return to Article Details Peridotitic diamond formation at Panda (Slave craton, Canada) from paleo-subduction wedge- or mantle-derived fluids ? The bearing of stable isotope data (15N/14N, 33S/32S, 34S/32S, /12C) Download Download PDF