Late Ordovician to Silurian evolution of Eastern Avalonia during Iapetus closure.

Woodcock, N. H. (2012) Late Ordovician to Silurian evolution of Eastern Avalonia during Iapetus closure. In: Geological History of Britain and Ireland. Wiley-Blackwell, pp. 177-191. ISBN 978-1-4051-9381-8

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Abstract

This chapter contains sections titled: Palaeocontinental Setting: Eastern Avalonia Converges with Baltica and Laurentia Changes in Global Sea Level and Climate Large-Scale Stratigraphic Signatures Post-Volcanic Transgressions and Mud Blankets (Late Caradoc to Mid-Ashgill) Late Ordovician Tectonics Latest Ordovician Glacial–Eustatic Regression Early Silurian Post-Glacial Transgressions Silurian Volcanism Silurian Tectonic Controls Mid-Silurian Closure of Iapetus Late Silurian Soft Collision and Basin Shallowing Summary: Basin Formation and Shallowing During Iapetus Closure References

Item Type:	Book Section
Additional Information:	Related url contains link to student companion web site: http://www.wiley.com/go/woodcock/geologicalhistory
Uncontrolled Keywords:	2011AREP; IA63;
Subjects:	02 - Geodynamics, Geophysics and Tectonics
Divisions:	02 - Geodynamics, Geophysics and Tectonics
Page Range:	pp. 177-191
Identification Number:	https://doi.org/10.1002/9781118274064.ch11
Depositing User:	Sarah Humbert
Date Deposited:	23 Dec 2011 11:32
Last Modified:	23 Jul 2013 10:03
URI:	http://eprints.esc.cam.ac.uk/id/eprint/2315

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