Tertiary Basins of Spain: The Stratigraphic Record of Crustal Kinematics: World and Regional Geology, cartea 6
Editat de Peter F. Friend, Cristino J. Dabrioen Limba Engleză Paperback – 9 noi 2005
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Specificații
ISBN-13: 9780521021982
ISBN-10: 0521021987
Pagini: 420
Ilustrații: 400 maps
Dimensiuni: 210 x 280 x 27 mm
Greutate: 0.94 kg
Ediția:Revised
Editura: Cambridge University Press
Colecția Cambridge University Press
Seria World and Regional Geology
Locul publicării:Cambridge, United Kingdom
ISBN-10: 0521021987
Pagini: 420
Ilustrații: 400 maps
Dimensiuni: 210 x 280 x 27 mm
Greutate: 0.94 kg
Ediția:Revised
Editura: Cambridge University Press
Colecția Cambridge University Press
Seria World and Regional Geology
Locul publicării:Cambridge, United Kingdom
Cuprins
part of the northern Ebro basin margin, as indicated by its tertiary fluvial sedimentary fill; 23. The Rioja area (westernmost ebro basin); part west; part c centre; part s south.
Recenzii
'This is undoubtedly a mature source book, which provides a wealth of information, clearly expressed in an annotated text with beautiful diagrams. The references are timely. Another nice feature is the nicely interpreted seismic lines. … This professional book should be on the shelves of those interested in Spanish geology, and in the libraries of geology departments and exploration companies.' Christopher Kendall, The Leading Edge
'It undoubtedly provides the most extensive coverage of the Tertiary geology of Spain ... and is therefore essential reference material for anyone interested in the sedimentology, stratigraphy and tectonics of the region … This book is a 'must'.' Gary Nichols, Geological Magazine
'It undoubtedly provides the most extensive coverage of the Tertiary geology of Spain ... and is therefore essential reference material for anyone interested in the sedimentology, stratigraphy and tectonics of the region … This book is a 'must'.' Gary Nichols, Geological Magazine
Descriere
The first book to deal comprehensively with Spain's tectonic and sedimentary history over the past sixty or so million years.