24.04.2013 Views

Arkell.1956.Jurassic..

Arkell.1956.Jurassic..

Arkell.1956.Jurassic..

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

i8 THE BRITISH ISLES<br />

seldom a little more (Portsdown boring 1294 m.). Where normally<br />

developed, they show a marked tendency to cyclic lithology ; the tripartite<br />

sequence, clay, sand, limestone is repeated many times. Yorkshire<br />

and Scotland differ by having a deltaic development of most of the Middle<br />

Jurassic, but otherwise are essentially similar. The sand/sandstone<br />

member of the various cycles is always more or less diachronic, sometimes<br />

markedly so. The highest Upper Jurassic stages, the Upper Kimeridgian,<br />

Portlandian and Purbeckian, are present only in the south of England.<br />

They are perfectly conformable with one another and the Purbeckian<br />

passes up imperceptibly into the Wealden. In Lincolnshire and Yorkshire<br />

marine Neocomian rests transgressively on Kimeridge Clay<br />

(Swinnerton, 1935), and farther south, in places where the Wealden lake<br />

beds are absent, marine Aptian or even Albian rests transgressively or (as<br />

in Dorset) unconformably on various formations of the Upper Jurassic.<br />

Volcanic rocks are absent from the British Jurassic. Conglomerates<br />

are few, thin and altogether inconspicuous, except in the Lower<br />

Kimeridgian of East Scotland, close to an Old Red Sandstone shoreline<br />

(Bailey & Weir, 1932; Waterston, 1951). Internal unconformities are<br />

seldom so marked that they can be detected without mapping, but very<br />

gentle ones do exist, especially in the Bajocian of the Cotswolds. Disconformities<br />

are frequent. Besides the Middle Jurassic deltaic beds in<br />

Scotland and Yorkshire there are beds of partly 'estuarine' facies in the<br />

Bathonian of the Midlands and a thin brackish or freshwater bed with<br />

Viviparus in the Bathonian of Oxfordshire. The Purbeckian is largely<br />

brackish and partly lacustrine. Liassic shorelines exist in South Wales<br />

and round the Mendips and neighbouring hills, which were an archipelago<br />

in the Lower Jurassic sea.<br />

Summaries and revisions of many areas have been published since<br />

1933. The principal ones are as follows:—<br />

General lie of the Jurassic of England: Lees & Taitt, 1946; Kent,<br />

1947, 1949; White, 1949.<br />

Dorset: Kellaway & Wilson, 1941; Chatwin, 1948; Arkell, 1947,<br />

1951a, 1951&.<br />

Cotswolds: Gardiner & others, 1934; Richardson, 1933; Cox, 1941,<br />

1950; Kellaway & Welch, 1948; Channon, 1950.<br />

Oxford district: Arkell, Richardson & Pringle, 1933; Richardson &<br />

others, 1946; Arkell, 19396, 1943, 1944, 1947a.<br />

East Midlands: Richardson, 1938-40; Hollingworth & others, 1944;<br />

Hollingworth & Taylor, 1946, 1951; Edmunds & Oakley,<br />

1947; Kent, 1947; Wilson, 1948; Whitehead & others, 1952.<br />

Lincolnshire: Richardson, 1938-40; Kent, 1941; Swinnerton & Kent,<br />

1949; Wilson, 1948a; Evans, 1952.<br />

Yorkshire: Wilson, Hemingway & Black, 1934; Rastall &<br />

Hemingway, 1940-49; Smithson, 1934, 1942; Wilson, 1936, 1938,<br />

1948a; Arkell, 1945; Sylvester-Bradley, 1953.<br />

Scotland: Macgregor, 1934; Waterston, 1951.<br />

http://jurassic.ru/

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!