Hostname: page-component-cd9895bd7-dk4vv Total loading time: 0 Render date: 2024-12-24T16:31:21.776Z Has data issue: false hasContentIssue false
  • English
  • Français

The Relationship of the Pilton Beds of North Devon to their Equivalents on the Continent

Published online by Cambridge University Press:  01 May 2009

Henry Paul
Henry Paul
Affiliation:
Essen
Get access Rights & Permissions [Opens in a new window]

Extract

Having made a general study of the Devonian-Carboniferous junction in North-West Europe and a more detailed one of special areas, the author discusses here the correlation of the Pilton Beds of North Devonshire and the “K beds” of the Bristol and Forest of Dean areas with the Etroeungtian and other horizons near the Devonian-Carboniferous boundary on the Continent.

Type
Original Articles
Information
Geological Magazine , Volume 74 , Issue 10 , October 1937 , pp. 433 - 442
Copyright
Copyright © Cambridge University Press 1937

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

LITERATURE

Delépine, G. 1911. “Recherches sur le Calcaire carbonifère de la Belgique,” Mém. et Trav. pulb. p. l. profess, des Faeult. Cath. de Lille.Google Scholar
Delépine, G. 1921. “Les couches de la base du Calcaire carbonifère dans la vallée de la Dendre,” Ann. Soc. géol. Nord., xlvi, 45–54.Google Scholar
Delépine, G. 1923. “Note sur la présence à Florennes (Belgique) de calcaires de la Zone d' Etroeungt,” Ann. Soc. géol. Nord., xlviii, 132–5.Google Scholar
Vaughan, A. 1915. “Correlation of Dinantian and Avonian,” Quart. Journ. Geol. Soc., lxxi, 1.CrossRefGoogle Scholar
Dantz, C. 1893. “Der Kohlenkalk der Umgebung von Aachen,” Zeitschr. d. Deutsch. Geol. Gesellsch., xlv, 594.Google Scholar
Paul, Henry. 1937. “Die Transgression der Viséstufe am Nordrande des Rheinischen Schiefergebirges,” Abhandl. Preuss. Geol. Landesanst. N.F., Heft 179.Google Scholar
Drevermann, F. 1902. “Ueber eine Vertretung der Etroeungtstufe auf der rechten Rheinseite,” Zeitschr. d. Deutsch. Geol. Gesellsch.Google Scholar
Kayser, E. 1882. “Beiträge zur Kenntniss von Oberdevon und Culm am Nordrande des rheinischen Sehiefergebirges,” Jahrbuch der königl. preuss. Geol. Landesanst. für 1881.Google Scholar
Paul, Henry. 1935. Vergleich des nordwestdeutschen Unterkarbon mit dem belgischen, Heerlen Congress.Google Scholar
Evans, J. W. 1919. “The Correlation of the Devonian Rocks of North Devon with those of other localities,” Geol. Mag., LVI, 547–9.Google Scholar
Paul, Henry. 1936. “Die Transgression der Viséstufe in Nordwesteuropa,” Decheniana, Bonn, 241.Google Scholar
Richter, Rud and Emma, . 1933. “Die letzten Phacopidae,” Bull. Musée Royal d' Hist. Nat. de Belgique, ix, no. 21, 1–19, pl. 1–2.Google Scholar
Vaughan, A., 1905. “The Palaeontological Sequence in the Carboniferous Limestone of the Bristol Area,” Quart. Journ. Geol. Soc., lxi, 181–307.CrossRefGoogle Scholar
Whideorne, S. F. 1896. A Monograph of the Devonian Fauna of the South of England. Vol. iii: The Fauna of the Marwood and Pilton Beds, Palaeontogr. Soc., London.Google Scholar
Carpentier, A. 1913. “Contribution a l' Étude du Carbonifère du Nord de la France,” Mém. Soc. géol. Nord., vii, ii.Google Scholar
Dehèe, R. 1929. “Description de la Faune d' Etroeungt. Faune de Passage du Dévonien au Carbonifère,” Mém. Soc. géol. France, N.S., v.Google Scholar
Delèpine, G. 1929. “Sur la présence de Cymaclymenia camerata Schindewolf dans la zone d' Etroeungt à Semeries (Nord de la France),” Ann. Soc. géol. Nord., liv, 99–107, pl. vi.Google Scholar
Gosselet, J. 1888. L' Ardenne.Google Scholar
Le Mattre, Mlle D. 1933. “Description des Stromatoporoides de l' Assise d' Etroeungt,” Mém. Soc. géol. France, N.S., ix.Google Scholar