๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

Sedimentation and tectonics in the Welsh Basin: Introduction

โœ Scribed by W. R. Fitches; N. H. Woodcock


Publisher
John Wiley and Sons
Year
1987
Tongue
English
Weight
312 KB
Volume
22
Category
Article
ISSN
0072-1050

No coin nor oath required. For personal study only.

โœฆ Synopsis


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 meeting were offered for publication. A report of the full proceedings has appeared in the Journal of the Geological Society (Fitches and Woodcock 1986) as have abstracts of all the contributions.

The stimulus for the conference was the recent upsurge in structural and sedimentological research in Wales, following and partly stimulated by new work on Welsh volcanic rocks (reviews by Allen 1982; Bevins et al. 1984; Kokelaar et al. 1984). The papers here reflect the breadth as well as the quantity of the activity, particularly in previously underresearched areas such as the Mid Welsh Late Ordovician to Early Silurian sedimentary rocks.


๐Ÿ“œ SIMILAR VOLUMES


Late Silurian (Ludlowโ€“Pล™รญdolรญ) microfoss
โœ C. Giles Miller; Stuart J. E. Sutherland; Ken J. Dorning ๐Ÿ“‚ Article ๐Ÿ“… 1997 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 565 KB

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 (Prร รตร‚ dolรตร‚ Series, upper Silurian) on the basis of brachiopod, bivalve, gastropod and ostracod faunas. The detailed distribution of microfossil

Wenlock volcanism in the Welsh Basin
โœ Richard Cave; David K. Loydell ๐Ÿ“‚ Article ๐Ÿ“… 1998 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 796 KB

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