Hostname: page-component-5c6d5d7d68-wp2c8 Total loading time: 0 Render date: 2024-08-19T12:08:51.086Z Has data issue: false hasContentIssue false

VI.—The Carboniferous Limestone of the Wrekin District

Published online by Cambridge University Press:  01 May 2009

Extract

The Carboniferous Limestone cropping out near Wellington and near Newport in the Wrekin district has hitherto received little attention. One or two references to the Lower Carboniferous rocks of the area are made in Geology in the Field, in which the limestone is referred to the Dibunophyllum zone, and the intrusive material underlying the limestone is described as an olivine-dolerite, probably of Tertiary age. Apart from these references there does not appear to be any published description of the limestone of the district. Although the Lower Carboniferous outcrops in the area are small, the faunal contents, stratigraphical horizon, and petrology of these rocks are subjects of interest in connection with recent work on the Carboniferous Limestone of various Midland districts.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1919

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

page 77 note 1 Geology in the Field, p. 762.

page 77 note 2 Idem, p. 766

page 80 note 1 Q.J.G.S., 1908.Google Scholar

page 80 note 2 For this and other analyses I am indebted to Mr. H. A. Doy.