The Position of the Wenlock/Lundlow Boundary in the Silurian Graptolite Sequence
- 1 June 1967
- journal article
- other
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 104 (4) , 395-397
- https://doi.org/10.1017/s0016756800048986
Abstract
No abstract availableThis publication has 5 references indexed in Scilit:
- The Salopian Graptolite Shales of the long mountain and similar rocks of Wenlock edgePublished by Elsevier ,2008
- Pristiograptus ludensis (Murchison 1839)—Its Synonymy and Allied Species—and the Position of the Wenlock/Ludlow Boundary in the Silurian Graptolite SequenceGeological Magazine, 1966
- The Aymestry Limestone of the Main OutcropQuarterly Journal of the Geological Society, 1936
- The Lower Ludlow Formation and its Graftolite-FaunaQuarterly Journal of the Geological Society, 1900
- II.—Notes on the Physical Character and Thickness of the Upper Silurian Rocks of Shropshire, with the Brachiopoda they Contain grouped in Geological HorizonsGeological Magazine, 1881