Anbieter: Anybook.com, Lincoln, Vereinigtes Königreich
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In den WarenkorbZustand: Poor. Volume 12. This is an ex-library book and may have the usual library/used-book markings inside.This book has soft covers. In poor condition, suitable as a reading copy. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,1350grams, ISBN:9780632030170.
Anbieter: Anybook.com, Lincoln, Vereinigtes Königreich
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In den WarenkorbZustand: Good. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. Clean from markings. In good all round condition. No dust jacket. Re-bound by library. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,1500grams, ISBN:9780632030170.
Sprache: Englisch
Verlag: London : Geological Society, 2018
ISBN 10: 1786203960 ISBN 13: 9781786203960
Anbieter: Joseph Burridge Books, Dagenham, Vereinigtes Königreich
EUR 238,67
Anzahl: 2 verfügbar
In den WarenkorbHardcover. Zustand: New. 384 pages. Cratonic basins are large, distinctive features of the continental crust. They are preferentially developed on thick continental lithosphere, are typically sub-circular in shape and subside over periods of hundreds of millions of years. They are also endowed with significant resources. However, in spite of their location in continental interiors and often well-known geology, the subsidence driving mechanism and tectonic setting of these basins remains controversial. This volume presents both lithospheric and basin scale datasets acquired specifically to interrogate the tectonic process of cratonic basin formation. Focused on the Silurian to Triassic Parnaíba cratonic basin of Brazil, the papers discuss the results of a multidisciplinary basin analysis project comprising new geophysical, geological and geochemical data. This unique dataset enables the characterization of the lithospheric crust and mantle beneath the Parnaíba Basin, constrains the detailed evolution of the basin itself, and enables comparisons with cratonic basins globally. Several convergent themes emerge providing new and powerful constraints for models of the driving mechanisms of these enigmatic basins.