A ~ 200 km thick layer surrounding the fluid core of the Earth occupying the lowermost mantle. D" had been defined by Keith Bullen (1950) and is believed to be a region of strong thermal and chemical heterogeneity. See: Lay (2002)
Peter Bormann, Keiiti Aki, William H. K. Lee, and Johannes Schweitzer (Compilers and Amenders), Glossary of Terms Interest to Earthquake and Engineering Seismologists (Version 1), Publication records from external use of GFZ scientific infrastructure, Germany 2011. http://gfzpublic.gfz-potsdam.de/pubman/item/escido c:56137:3/component/escidoc:56143/Glossary_rev1.pd f, (ND/ Erthq - Amer) {980}