This book sheds valuable new light on the genetic mineralogy of lower-mantle diamonds and
syngenetic minerals. It presents groundbreaking experimental results revealing the melting
relations of ultrabasic and basic associations and a physicochemical peritectic mechanism of
their evolution. The experimental investigations included here reveal the key multicomponent
multiphase oxide-silicate-carbonate-carbon parental media for lower-mantle diamonds and
syngenetic minerals. Consequently readers will find extensive information on the
diamond-parental oxide-silicate-carbonate-carbon melts-solutions that supplement the general
features of lower-mantle diamond genesis and the most efficient ultrabasic-basic evolution. The
experimental results on physicochemical aspects combined with analytical mineralogy data make
it possible to create a generalized composition diagram of the diamond-parental melts-solutions
there by completing the mantle-carbonatite concept for the genesis of lower-mantle diamonds and
syngenetic minerals. This book addresses the needs of all researchers studying the Earth¿s
deepest structure super-deep mineral formation including diamonds and magmatic evolution.
