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Quarterly Journal of Engineering Geology and Hydrogeology

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Quarterly Journal of Engineering Geology and Hydrogeology; 2003; v. 36; issue.3; p. 287-288;
DOI: 10.1144/1470-923/00926
© 2003 Geological Society of London

Book review

L.J. Donnelly

The first 250 words of the full text of this article appear below. Images appear only in PDF or full-text views.

Magmatism and Geodynamics: Terrestrial Magmatism Throughout the Earth's History. O. A. Bogatikov (ed). Gordon & Breach, 2000, hardback; xiiii+511pp. ISBN 90-5699-168-X.

This book has been translated from Russia and the discussions presented, mainly based on data from the former USSR and neighbouring countries, have not been previously available to non-Russian readers. This research was undertaken in 1984–1988 at the Instituteof Ore Deposits Geology, Petrology, Mineralogy and Geochemistry (IGEM) at the Russian Academy ofScience, in Moscow.

This book provides geochemical, petrochemical, isotopic and petrological data and discussions on magmatic evolution and igneous processes, deep-seated petrogenesis, geodynamic environments and the interrelationships between magmatism and tectonics, throughoutthe stages of crustal evolution; during the Archaean, Proterozoic and Phanerozoic, up to the present day.

The first chapter discusses the solidification, fractional crystallization and petrogenesis of igneous melts. This is followed by three chapters dedicated to plate tectonics including, magmatism at divergent and convergent plate boundaries, intraplate and recent magmatism, the origin of fold belts and anorogenic magmatism. The majority of the book concentrates on magmatic processes which were active during the Archaean and Proterozoic, and discusses the evolution of the Earth's lithosphere from a primordial magmatic crust, through four stages; lunar (pre-geological), nuclearic (primitive crustal) cratonic stage (granulite-greenstone terranes and granulite–granitefold belts) and Continental–Oceanic (Plate Tectonics). According to the authors, Plume Tectonics dominated the first three stages, with the present day Plate Tectonic regime only starting 2 Ga ago. The final two chapters of the book discuss terrestrial and lunar magmatism and the sources, origins . . . [Full Text of this Article]