The collection of papers in this volume results from a joint meeting of the Tectonic Studies Group and the British Sedimentological Research Group of the Geological Society of London, held at the University College of Wales, Aberystwyth on 10-12 April 1986. About half the papers presented at that me
Wenlock volcanism in the Welsh Basin
✍ Scribed by Richard Cave; David K. Loydell
- Publisher
- John Wiley and Sons
- Year
- 1998
- Tongue
- English
- Weight
- 796 KB
- Volume
- 33
- Category
- Article
- ISSN
- 0072-1050
No coin nor oath required. For personal study only.
✦ Synopsis
Within the Welsh Basin, proximal volcanism of Wenlock age is virtually unknown. However, two vitroclastic tus and a turbiditic tuaceous mudstone have been discovered lying along the eastern side of the basin. Their sources have not been located, but the tuaceous mudstone and the older tu are both of riccartonensis Zone age and may be the products of the same event. The younger tu is of early ludensis Zone age. All three occur in association with bentonites and represent, or were involved in, sedimentary instability.
📜 SIMILAR VOLUMES
Intraplate volcanism in the Central Indian Ocean Basin (CIOB) has been of much interest, since this tectonically young and structurally complex basin holds signatures of at least one major plate reorganisation at 65 š 5 Ma; and two major plate boundary structural deformations occurring at 54:5 š 3 M
## Abstract With volume ratio of 8:1:1.5 amongst acidic, intermediate and basaltic rocks, the Cretaceous volcanics around the Songliao Basin are a series of high‐K or medium‐K, peraluminous or metaluminous, calc‐alkaline rocks, lacking typical basalts and peralkaline members of typical rift‐related
The base of the Clun Forest Formation at Clun, Shropshire, has previously been taken to correlate with the base of the Downton Castle Sandstone Formation (PrÏ õÂ dolõÂ Series, upper Silurian) on the basis of brachiopod, bivalve, gastropod and ostracod faunas. The detailed distribution of microfossil
## Abstract Inversion of the Lower Palaeozoic Welsh Basin during the Early to Mid‐Devonian is generally thought to have been achieved by a combination of approximately co‐axial shortening and transcurrent movement along major faults to produce a strongly partitioned transpressional strain. However,