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Originally published in 1963, this classic textbook was revised fully for the 1972 edition. The author presents a comprehensive account of all topics falling within the domain of structural geology in his characteristically objective, scientific and logical manner. The book pays particular attention to definitions and the origin of terms. Geology is a global science and this book used examples and ideas from work in many countries. The book is comprehensive in scope, dealing not only with secondary structures and tectonics, but also with primary structures of secondary and igneous rocks. This was the first textbook to deal with rock material as two-phase systems rather than as solids and this approach is continued in this reissued edition by analysis of concepts such as ocean-floor spreading and plate tectonics
Focusing on mountain ranges that are relatively unfamiliar to most geologists, this work expands our view of tectonics beyond a standardized textbook approach and illustrates both the extraordinary variety of mountain ranges over the world through time and many of the basic similarities they display. Originally published in 1987. The Princeton Legacy Library uses the latest print-on-demand technology to again make available previously out-of-print books from the distinguished backlist of Princeton University Press. These editions preserve the original texts of these important books while presenting them in durable paperback and hardcover editions. The goal of the Princeton Legacy Library is to vastly increase access to the rich scholarly heritage found in the thousands of books published by Princeton University Press since its founding in 1905.
This volume summarizes the state of the art of Variscan geology from Iberia to the Bohemian Massif. The European Variscan belt consists of two orogens: the older, northern and the younger, southern. The northern Variscan realm was dominated by Late Devonian–Carboniferous rifting, subduction and collisional events as defined by sedimentary records, crustal growth, recycling of continental crust and large-scale deformations. In contrast, the southern European crust was reworked by major Late Carboniferous collision followed by Permian wrenching. The Late Carboniferous–Permian orogeny overprinted the previously accreted system in the north, but with much lower intensity, resulting in magmatic recycling and extensional tectonics. These two main orogenic cycles do not reflect episodic evolution of a single orogenic system but a complete change in orientation of stress field, thermal regime, degree of reworking and recycling of European crust, reflecting a major switch in plate configurations at the Early–Late Carboniferous boundary.

Proceedings

Koninklijke Nederlandse Akademie van Wetenschappen. Afdeling Natuurkunde

Published: 1977

Total Pages:


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