Construction of an evolutionary deglaciation model for the Irish midlands based on the integration of morphostratigraphic and geophysical data analyses
Version of Record online: 21 AUG 2012
Copyright © 2012 John Wiley & Sons, Ltd.
Journal of Quaternary Science
Volume 27, Issue 8, pages 807–818, November 2012
How to Cite
Pellicer, X. M., Warren, W. P., Gibson, P. and Linares, R. (2012), Construction of an evolutionary deglaciation model for the Irish midlands based on the integration of morphostratigraphic and geophysical data analyses. J. Quaternary Sci., 27: 807–818. doi: 10.1002/jqs.2570
- Issue online: 14 NOV 2012
- Version of Record online: 21 AUG 2012
- Manuscript Accepted: 25 JUN 2012
- Manuscript Revised: 21 JUN 2012
- Manuscript Received: 9 JAN 2012
Additional supporting information may be found in the online version of this article.
|jqs_2570_sm_SuppFigS1.jpg||1168K||Figure S1. Exposure in deformed interstratified glaciofluvial sand and gravel, dipping NNE, deposited on a kame terrace positioned along the north-west slope of Croghan Hill.|
|jqs_2570_sm_SuppFigS2.jpg||1466K||Figure S2. Cross-section of glaciolacustrine sediments overlying Clara Esker ridge.|
|jqs_2570_sm_SuppFigS3.jpg||2171K||Figure S3. Exposure in the Ballyduff Esker complex and longitudinal profile of Ballyduff Esker ridge.|
|jqs_2570_sm_SuppFigS4.jpg||917K||Figure S4. Inverse model of the pseudosection for ERT profiles RS8-L1-10m and RS8-L2-10m and interpretation of the datasets.|
|jqs_2570_sm_SuppTabS1.docx||14K||Table S1 Lithofacies coding scheme used for interpretation of exposures, modified from Benn and Evans (1998).|
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