Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/85575
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Type: Journal article
Title: Comment on 'Crustal structure of the British Isles and its epeirogenic consequences' by M.W Davis, N.J. White, K.F. Priestley, B.J. Baptie and F.J. Tilmann
Author: Hillis, R.
Holford, S.
Green, P.
Dore, A.
Gatliff, R.
Stoker, M.
Turner, J.
Underhill, J.
Williams, G.
Citation: Geophysical Journal International, 2013; 194(2):678-679
Publisher: Blackwell Publishing
Issue Date: 2013
ISSN: 0956-540X
1365-246X
Statement of
Responsibility: 
Richard R. Hillis, Simon P. Holford, Paul F. Green, Anthony G. Doré, Robert W. Gatliff, Martyn S. Stoker, Jonathan P. Turner, John R. Underhill and Gareth A. Williams
Abstract: While Davis et al. provide convincing evidence for dynamic support of modern topography in NW Scotland, we take issue with their claims that the spatial distribution of Cenozoic denudation correlates poorly with the pattern of upper crustal shortening, and that the magnitude of shortening is insufficient to cause the observed denudation. We disagree with Davis et al.'s map of denudation, which forms the basis of their claims, and believe that their conclusions seriously downplay the widely documented contribution of crustal shortening to Cenozoic denudation of many areas of the British Isles.
Rights: © The Authors 2013
RMID: 0020137162
DOI: 10.1093/gji/ggt139
Appears in Collections:Australian School of Petroleum publications

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