Author:
Reading H. G.,Poole A. B.
Abstract
AbstractThe paper describes an unconformable junction of Upper Llandovery upon Malvernian in the Gullet Quarry of the South Malvern Range and discusses the evidence for and the significance of other comparable junctions in the Malverns. It is considered that Taconic movements are a factor in Malvern tectonics and that the importance of a “ western boundary fault ” to the Malvernian has been overstressed in the past.
Publisher
Cambridge University Press (CUP)
Reference14 articles.
1. The Geological Structure of the Southern Malverns, and of the Adjacent District to the West
2. On the Geological Structure of Portions of the Malvern and Abberley Hills
3. The Malvern hills compared with the Palaeozoic districts of Abberley, etc;Phillips;Mem. Geol. Surv.,1848
4. The geology of Malvernia;Bennett;Malvern Naturalists' Field Club,1942
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