A suitable reduction velocity mostly used for controlled-source P wave crustal studies is 6 km/sec, for upper-mantle studies 8 km/sec, for S wave studies the reduction velocity is usually that for P wave studies divided by √3
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}