“…Of special interest are secondary corundum deposits that are associated with rift-related alkaline basaltic volcanism as these are among the world's largest gem corundum suppliers (e.g., Guo et al 1996;Limtrakun et al 2001;Shore and Weldon 2009) and are hence economically of great importance. Such basaltic secondary deposits are located all over the world, most notably in Asia (e.g., Guo et al 1996, and in eastern Australia, at the western Pacific margin (e.g., Coenraads 1990;Graham et al 2008;Sutherland 1996;Sutherland et al 1998aSutherland et al , 2002Sutherland et al , 2009bSutherland et al , 2015Sutherland et al , 2017Saminpanya 2001;McGee 2005;Abduriyim et al 2012), but also in Europe (e.g., Malikova 1999;Giuliani et al 2009;Uher et al 2012), Africa (Kiefert and Schmetzer 1987;Krzemnicki et al 1996;Schwarz et al 2000;Pardieux et al 2014), in South America , and in North America (e.g., Garland 2002;Berg 2007Berg , 2014Palke et al 2017).…”