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British Stratigraphy: Introducing Geology Series, cartea 2

Autor Frank A. Middlemiss
en Limba Engleză Paperback – 31 dec 1974
This book is primarily intended to assist candidates studying geology for the Ordinary Level of G.c.E., and examinations of comparable standard, but it should also be found useful by the" reader requiring a rapid conspectus of the geological history of Britain, and as forming a basis for more advanced work. The scope of the subject matter necessitated a narrow and slippery path be­ tween over-simplification and excessive detail, but the balance adopted is based upon the experience of many years of teaching at all levels, and of examining for the London G.C.E. Board. The maps, combining outcrop dis­ tribution with palaeogeography, presented some difficulty, especially for periods of continuously changing geography, such as the Cretaceous. It was necessary in these cases to make an arbitrary choice of one small part of the period, the geography of which could be illustrated. Candidates are advised not to spend time learning every detail of the outcrop patterns, but to con­ centrate upon the main areas of outcrop. I am indebted to Mrs. Jean Fyffe for the cartographic work.
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Specificații

ISBN-13: 9780045500239
ISBN-10: 0045500231
Pagini: 49
Ilustrații: 49 p. 25 illus., 24 illus. in color.
Dimensiuni: 189 x 246 x 3 mm
Greutate: 0.12 kg
Ediția:1974
Editura: SPRINGER NETHERLANDS
Colecția Springer
Seria Introducing Geology Series

Locul publicării:Dordrecht, Netherlands

Public țintă

Research

Cuprins

1 Geological History.- 2 The Pre-Cambrian Era.- 3 The Lower Palaeozoic Geosyncline.- 4 The Caledonian Mountain-building.- 5 Devonian Environments.- 6 The Lower Carboniferous Marine Transgression.- 7 The Upper Carboniferous Deltas and Coal Swamps.- 8 The Armorican Mountain-building.- 9 The Permo-Triassic Desert Environment.- 10 The Fluctuating Shelf-seas of the Jurassic.- 11 The Cretaceous Marine Transgression.- 12 Tertiary Cycles of Sedimentation and Igneous Activity.- 13 The Alpine Mountain-Building and the Later Tertiary.- 14 The Quaternary Glaciations.