A late Ordovician (Hirnantian) karstic surface in a submarine channel, recording glacio-eustatic sea-level changes: Meifod, central Wales

Author:

Brenchley Patrick J.,Marshall Jim D.,Harper David A. T.,Buttler Caroline J.,Underwood Charlie J.

Publisher

Wiley

Subject

Geology

Reference32 articles.

1. Deep-sea sediments record the geophysiology of the late Ordovician glaciation

2. 1988. Environmental changes close to the Ordovician boundary. In A Global Analysis of the Ordovician-Silurian Boundary, (eds). Bulletin of the British Museum of Natural History (Geology) 43: 377-385.

3. 1992. Ordovician (Caradoc), Southern British Isles. In Atlas of Palaeogeography and Lithofacies, , (eds). Geological Society Memoir 13: 28-32.

4. 1993. The Ordovician of the south Berwyn Hills. In Geological Excursions in Powys, Central Wales, (eds). University of Wales Press: Cardiff; 39-50.

5. . 1984. The environmental distribution of associations belonging to the Hirnantia fauna-evidence from North Wales and Norway. In Aspects of the Ordovician System, (ed.). Palaeontological Contributions from the University of Oslo 295: 113-125.

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