Hostname: page-component-848d4c4894-wzw2p Total loading time: 0 Render date: 2024-05-16T02:25:36.644Z Has data issue: false hasContentIssue false
  • English
  • Français

The Faunal Sequence in the Kent Coalfield

Published online by Cambridge University Press:  01 May 2009

C. J. Stubblefield  and
A. E. Trueman
Get access Rights & Permissions [Opens in a new window]

Extract

A Summary of the stratigraphy of the Coal Measures in the Kent Coalfield was given by H. G. Dines in 1933, accompanied by notes on the fossil flora by R. Crookall and on the fauna by C. J. Stubblefield. It was shown that the Coal Measures could be divided into a Lower or Shale Division, some 700 feet thick, consisting mainly of shales with some thick coals, and an Upper or Sandstone Division, about 2,100 feet thick, consisting mainly of sandstone with a few mostly impersistent coal seams, except in the highest part where again there are shales with coals (Dines, 1933, p. 22); the dividing line was taken at the base of a sandstone usually about 100 feet below the Millyard Seam. Recently the correlatable seams in the coalfield have been designated by means of numbers in downward succession and seams numbered 1–6 lie in the Sandstone Division, and numbers 7–14 in the Shale Division (Dines, 1945). R. Crookall regarded the Upper or Sandstone Division as representing the StafFordian and part of the Radstockian series, while the Shale Division he referred to the Yorkian (Text-fig. 1).

Type
Articles
Information
Geological Magazine , Volume 83 , Issue 6 , December 1946 , pp. 266 - 279
Copyright
Copyright © Cambridge University Press 1946

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Baker, H. A. 1935. An undiscovered Coalfield. Probability of its existence beneath North Kent, the Thames Estuary and south-east Essex. Iron and Coal Trades Review, 13th, 20th, 27th September (12 pp.).Google Scholar
Bolton, H. 1915. The Fauna and Stratigraphy of the Kent Coalfield. Trans. Inst. Mining Eng., xlix, pt. 4.Google Scholar
Corsin, P. 1932. Guide Paléontologique dans le Terrain Houiller du Nord de la France. Trav. et Mém. de I’Université de Lille, Albums Fasc. no. 5, 44 pp., pis. A-C, i-xl.Google Scholar
Crookall, R. 1933. Contributions to the Geology of the Kent Coalfield. (II) The Fossil Flora of the Kent Coalfield. Summ. Prog. Geol. Surv. for 1932, pt. ii, 44–70.Google Scholar
Demanet, F. 1943. Les Horizons marins du Westphalien de la Belgique et leurs faunes. Mém. Mus. R. d’Hisl. Nat. Belgique, no. 101, 166 pp., 9 pls.Google Scholar
Dines, H. G. 1933. Contributions to the Geology of the Kent Coalfield. (I) The Sequence and Structure of the Kent Coalfield. Summ. Prog. Geol. Surv. for 1932, pt. iii, 1933, 15–43.Google Scholar
Dines, H. G. 1945. (b) Report of the Geological Survey in Kent Coalfield Regional Survey Report Ministry of Fuel and Power, pp. 7–25.Google Scholar
Jongmans, W. J. 1940. Die Kohienfelder von Gross Britannien, Kent Kohlen-feld. Meded. behoorende bij het Jaarsverlag over 1938 en 1939. Geol. Sticht. Geol. Bureau voor het Mijngebiet te Heerlen. pp. 15–36.Google Scholar
Mitchell, G. H., Stubblefield, C. J., and Crookall, R. 1942. The Geology of the Warwickshire Coalfield. Wartime Pamphlet No. 25 (Geol. Surv.), 40 pp.Google Scholar
Pruvost, P. 1937. Discussion to Dix, E. and Trueman, A. E. The Value of Non-marine Lamellibranchs for the Correlation of the Upper Carboniferous. C.R., deuxiéme Congrés pour l’Avancement des Études de Stratigraphie Carbonifére, Heerlen, Septembre, 1935, Tome I, p. 199.Google Scholar
Renier, [A.]. 1937. In W. J. Jongmans and W. Gothan, Betrachtungen über die Ergebnisse des Zweiten Kongresses fiir Karbonstratigraphie. Ibid., p. 15.Google Scholar
Stubblefield, C. J. 1933. Contributions to the Geology of the Kent Coalfield. (III) Notes on the Fauna of the Coal Measures of Kent. Summ. Prog. Geol. Surv. for 1932, pt. ii, 1933, 71–77.Google Scholar
Stubblefield, C. J. 1941. Discussion to E. Dix. The General Sequence of Strata in the Warwickshire Coalfield. Abstr. Proc. Geol. Soc., no. 1382, p. 8.Google Scholar
Trueman, A. E. 1933. A suggested Correlation of the Coal Measures of England and Wales. Proc. S. Wales Inst. Eng., xlix, 63–94.Google Scholar
Trueman, A. E. 1946. Stratigraphical Problems in the Coal Measures of Europe and North America. Proc. Geol. Soc., cii, p. xlix.Google Scholar
Trueman, A. E. and Weir, J. 1946. A Monograph of British Carboniferous Non-marine Lamellibranchia, pt. i, pp. i-xxxii, 1–18, pis. i-iv. Palaeont. Soc. for 1945.Google Scholar
Waterlot, G. 1933. Les Productids du Terrain houiller du Nord de la France. Ann. Soc. du Nord for 1932, lvii, 145–176, pis. ii-iv.Google Scholar
Wray, D. A. and Trueman, A. E. 1931. The Non-marine Lamellibranchs of the Upper Carboniferous of Yorkshire and their zonal sequence. Summ. Prog. Geol. Surv. for 1930, pt. iii, 1931, 70–92.Google Scholar