Many interesting and perplexing questions arise in connection with the
highly potassic volcanic associa- tion dominated by mafic and ultramafic
rocks contain- ing leucite. Its occurrence is very restricted as compar-
ed with the olivine-basalt trachyte kindred, but it is distributed at
widely scattered points on all the conti- nents, and its chemical and
petrographic individuality is both remarkable and constant. A
considerable litera- ture is available related to the mineralogy,
petrology, geochemistry, phase chemistry, distribution, and origin of
this interesting suite of rocks. It seemed that there was a genuine need
for a review-synthesis of all these data, which would be intelligible to
a wide spectrum of advanced students and professionals in the earth
sciences. The monograph may be divided into two parts. The first part
consists of six chapters in which the mineralogical and chemical
peculiarities of leucite- bearing rocks and their nomenclature,
petrology, min- eralogy, distribution, and physical and chemical condi-
tions of formation are discussed. Phase equilibria stud- ies on many
leucite-bearing ternary, pseudoternary, quaternary, and pseudoquaternary
joins and systems, studied by different investigators at variable
tempera- tures in air, are described in the second part in Chap- ters 7
to 12. Survival of leucite and formation of pseu- doleucite is discussed
in Chapter 13. Leucite-bearing synthetic and natural rock systems
studied at different temperatures under variable pressures in presence
or absence of water, are summarized in Chapters 14 and 15.