Growth and decay of a marine terminating sector of the last British–Irish Ice Sheet: a geomorphological reconstruction-Reference-Cited by-同舟云学术

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Growth and decay of a marine terminating sector of the last British–Irish Ice Sheet: a geomorphological reconstruction

Published:2014-01 Issue: Volume:83 Page:28-45
ISSN:0277-3791
Container-title:Quaternary Science Reviews
language:en
Short-container-title:Quaternary Science Reviews

Author:

Finlayson Andrew,Fabel Derek,Bradwell Tom,Sugden David

Funder

British Geological Survey's (BGS) Geology and Landscape Scotland programme

BGS training

Publisher

Elsevier BV

Subject

Geology,Archeology,Archeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference96 articles.

1. Glaciootectonic Landforms and Structures;Aber,1989

2. A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements;Balco;Quat. Geochronol.,2008

3. The Loch Lomond Readvance on north Arran: glacier reconstruction and palaeoclimatic implications;Ballantyne;J. Quat. Sci.,2007

4. Clyde. 1:25,000 Series: Sea Bed Sediments and Quaternary Geology;B.G.S,1985

5. Flora, fauna and climate of Scotland during the Weichselian Middle Pleniglacial – palynological, macrofossil and coleopteran investigations;Bos;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2004

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3. Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction;Boreas;2022-09-07

4. Conserving Quaternary geoheritage in Northern Ireland;Proceedings of the Geologists' Association;2022-08

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