Hin, R CMorel, M.L.ANebel, OliverMason, P.R.D.van Westrenen, WimDavies, G R2015-12-130024-4937http://hdl.handle.net/1885/80293The ~533 Ma Venetia Diamond Mine is located between the Kaapvaal and Zimbabwe Cratons and the study of selected xenoliths provides the opportunity to investigate the temporal evolution of the sub-continental lithospheric mantle (SCLM) underneath southernKeywords: chemical composition; clinopyroxene; concentration (composition); craton; diamond; formation mechanism; garnet; lithospheric structure; magmatism; mantle structure; melting; metasomatism; peridotite; remobilization; rhenium-osmium dating; temporal variati Craton formation; Mantle lithosphere; MetasomatismFormation and temporal evolution of the Kalahari sub-cratonic lithospheric mantle: Constraints from Venetia xenoliths, South Africa200910.1016/j.lithos.2009.06.0202016-02-24