The origin of different kinds of igneous rocks can be understood in
terms of their tectonic setting, and by way of the isotope
compositions of strontium, neodymium, and lead. This book explains
the petrogenesis of igneous rocks as a consequence of tectonic
processes resulting from interactions between asthenopheric plumes
and the overlying lithospheric mantle. The relevant principles of
isotope geochemistry are explained in the first chapter, making it
accessible for university students as well as professionals. The
relevant isotopic data is presented in diagrammatic form. The book
contains more than 400 original drawings.
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