Journal of the Czech Geological Society PDF Download
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Author:
Publisher:
ISBN:
Category : Geology
Languages : cs
Pages : 298
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Author:
Publisher:
ISBN:
Category : Geology
Languages : cs
Pages : 298
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Author:
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ISBN:
Category : Earth sciences
Languages : en
Pages : 92
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Author: Martin Novák
Publisher:
ISBN:
Category :
Languages : en
Pages : 102
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Author: Martin Novák
Publisher:
ISBN:
Category : Geochemistry
Languages : en
Pages : 102
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Author: Česká geologická služba
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 40
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Author:
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ISBN:
Category :
Languages : en
Pages : 102
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Book Description
Author: Robert B. Blodgett
Publisher: Geological Society of America
ISBN: 0813724422
Category : Science
Languages : en
Pages : 338
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"Displaced or tectonostratigraphic terranes comprise a huge portion of real estate in the North American Cordillera. Terranes are discrete, fault-bound blocks of regional extent, with rocks and fossils that differ to a great extent from those of adjacent blocks. The allochthonous nature of most terranes, relative to adjacent craton, is well established. When mapped, they resemble a collage of mixed rock types, tectonic styles, metamorphism, and volcanic origins--each part resembling the pieces of a puzzle. Terrane studies remain integral to understanding the geological evolution of western North America. Since the initiation of the concept summarized in 1979 by the late David L. Jones, the significance of fossils and stratigraphy has been key to solving the puzzle. Chapters of this book written by experts in their field, provide a sense of the diversity of approaches in paleontology and stratigraphy. Contributions span geologic time from the Precambrian (Vendian) to Cretaceous and address over 20 Cordilleran terranes."--Publisher's website.
Author:
Publisher:
ISBN:
Category : Geology
Languages : cs
Pages : 418
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Author: K. Schulmann
Publisher: Geological Society of London
ISBN: 1862396582
Category : Science
Languages : en
Pages : 404
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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.
Author: Tom McCann
Publisher: Geological Society of London
ISBN: 9781862392465
Category : Science
Languages : en
Pages : 806
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Book Description
Volume 1 focuses on the evolution of Central Europe from the Precambrian to the Permian, a dynamic period which traces the formation of Central Europe from a series of microcontinents that separated from Gondwana through to the creation of Pangaea. Separate summary chapters on the Cadomian, Caledonian and Variscan orogenic events as well as on Palaeozoic magmatism provide an overview of the tectonic and magmatic evolution of the region. These descriptions sometimes extend beyond the borders of Central Europe to take in the Scottish and Irish Caledonides as well as the Palaeozoic successions in the Baltic region.