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The Evolution of the Rheic Ocean

The Evolution of the Rheic Ocean
Author: Ulf Linnemann
Publisher: Geological Society of America
Total Pages: 642
Release: 2007
Genre: Science
ISBN: 0813724236

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Geological evolution of middle to late Paleozoic rocks in the Avalon terrane of northern mainland Nova Scotia, Canadian Appalachians: a record of tectonothermal activity along the northern margin of the Rheic Ocean in the Appalachian-Caledonide orogen.


Origins

Origins
Author:
Publisher: University of Oklahoma Press
Total Pages: 372
Release: 2001
Genre: Nature
ISBN: 9780806133591

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Glorious panoramic photography by the author, a specialist in interpretive landscape, reveals the physical legacy of the Earth's distant past. This exceptional book celebrates the inevitability of global change and highlights our need as human beings to recognize and adjust to it. Color and b&w illustrations.


Earth History and Palaeogeography

Earth History and Palaeogeography
Author: Trond H. Torsvik
Publisher: Cambridge University Press
Total Pages: 329
Release: 2017
Genre: Science
ISBN: 1107105323

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This book provides a complete Phanerozoic story of palaeogeography, using new and detailed full-colour maps, to link surface and deep-Earth processes.


Geological History of Britain and Ireland

Geological History of Britain and Ireland
Author: Nigel H. Woodcock
Publisher: John Wiley & Sons
Total Pages: 433
Release: 2009-04-01
Genre: Science
ISBN: 1444311603

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Britain, Ireland and their surrounding areas have a remarkably varied geology for so small a fragment of continental crust. This region contains a fine rock record from all the geological periods from Quaternary back to Cambrian, and a less continuous but still impressive catalogue of events back through nearly 2500 million years of Precambrian time. This protracted geological history would have been interesting enough to reconstruct if it had been played out on relatively stable continental crust. However, Britain and Ireland have developed instead at a tectonic crossroads, on crust traversed intermittently by subduction zones and volcanic arcs, continental rifts and mountain belts. The resulting complexity makes the geological history of this region at once fascinating and perplexing. Geological History of Britain and Ireland tells the geological story of the region at a level accessible to undergraduate geologists, as well as to postgraduates, professionals or informed amateurs. The book takes a multi-disciplinary rather than a purely stratigraphical approach, and aims to bring to life the processes behind the catalogue of historical events. Full coverage is given to the rich Precambrian and Early Palaeozoic history, as well as to later events more relevant to hydrocarbon exploration. The book is profusely illustrated and contains guides to further reading and full references to data sources, making it an essential starting point for more detailed studies of the regional geology. All British Earth science undergraduates will be required to spend some time studying British Geological History, and this book will be the only one available to British undergraduates The book takes a process-based approach, rather than simply describing the regional stratigraphy Lavishly illustrated with high-quality diagrams


The Foundations and Birth of the Rheic Ocean

The Foundations and Birth of the Rheic Ocean
Author: Erdin Bozkurt
Publisher:
Total Pages: 163
Release: 2008
Genre: Continental drift
ISBN:

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Deals "with detailed aspects of palaeogeography, palaeontology, geochronology, provenance analysis, geochemistry, deformation and tectonics, magmatism and sedimentation, and are concerned with the evolution of Peri-Gondwanan correlatives from European, North and South America areas."--Page 1.


Pannotia to Pangaea

Pannotia to Pangaea
Author: B. Murphy
Publisher: Geological Society of London
Total Pages: 666
Release: 2021-01-28
Genre: Science
ISBN: 1786204924

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Special Publication 503 celebrates the career of R. Damian Nance. It features 27 articles, with more than 110 authors based in 18 different countries. These articles include contributions on the processes responsible for the formation and breakup of supercontinents, the controversies concerning the status of Pannotia as a supercontinent, the generation and destruction of Paleozoic oceans, and the development of the Appalachian-Ouachitan-Caledonide-Variscan orogens. In addition to field work, the approaches to gain that understanding include examining the relationships between stratigraphy and structural geology, precise geochronology, geochemical and isotopic fingerprinting, geodynamic modelling, regional syntheses, palaeogeographic modelling, and good old-fashioned arm-waving! The wide range of topics mirrors the breadth and depth of Damian’s contributions, interests and expertise. Like Damian’s papers, the contributions range from the predominantly conceptual to detailed field work, but all are targeted at understanding important tectonic processes. Their scope not only varies in scale from global to regional to local, but also in the range of approaches required to gain that understanding.


The Variscan Orogeny

The Variscan Orogeny
Author: K. Schulmann
Publisher: Geological Society of London
Total Pages: 404
Release: 2014-07-28
Genre: Science
ISBN: 1862396582

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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.