The rock types and successions encountered at two localities have been described and interpretated with reference to modern analogues. In the Clifton Down Limestone a cycle of sedimentation is recognised passing from intertidal algal mats, through lagoons, barrier and open shelf deposits and back th
The structure and non-calcareous residues of the Carboniferous Limestone of the Clitheroe area
โ Scribed by Arthur Bray
- Book ID
- 117120742
- Publisher
- The Geological Society (London)
- Year
- 1939
- Tongue
- English
- Weight
- 618 KB
- Volume
- 50
- Category
- Article
- ISSN
- 0016-7878
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๐ SIMILAR VOLUMES
The Pendleside Limestone is redefined as comprising the B, (S,) zone and the lower part of the B, (D,) zone. It is argued that the Bowland Shales, including the basal beds of upper B, age, transgress the Pendleside Limestone northwards from Clitheroe, following a shallow earth-movement with axes cro
This investigation of previously undescribed country along the Staffordshire-Derbyshire border indicated the need for reexamination of adjoining areas described in 1950 and 1951. The main revisions concern the ages of certain beds and the nature of the unconformities. Evidence is adduced of vertical