We use cookies to distinguish you from other users and to provide you with a better experience on our websites. Close this message to accept cookies or find out how to manage your cookie settings.
An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content.
Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)
References
Borradaile, G. J.1986. The internal tectonic fabric of minor intrusions and their potential as regional palaeostress indicators. Geological Magazine123, 665–71.CrossRefGoogle Scholar
Borradaile, G. J.1979. Strain study of the Caledonides in the Islay region, S.W. Scotland: implications for strain histories and deformation mechanisms in greenschists. Journal of the Geological Society of London136, 77–88.CrossRefGoogle Scholar
Cunningham-Craig, E. H., Bailey, E. B. & Wright, W. B.1911. The Geology of Colonsay and Oronsay with part of the Ross of Mull. Memoir. Geological Survey of the United Kingdom no. 35, 1–109.Google Scholar
Fitches, W. R. & Maltman, A. J.1984. Tectonic development and stratigraphy at the western margin of the Caledonides: Islay and Colonsay, Scotland. Transactions of the Royal Society of Edinburgh (Earth Sciences)75, 365–82.CrossRefGoogle Scholar
Peach, B. N., Wilkinson, S. B., Wright, W. B. & Maufe, H. B.1911. The Geology of Knapdale, Jura and North Kintyre. Memoir. Geological Survey of Scotland, no. 28, pp. 1–56.Google Scholar
Roberts, J. L.1974. The structure of the Dalradian rocks in the SW Highlands of Scotland. Journal of the Geological Society of London130, 93–124.CrossRefGoogle Scholar
Watson, J.1964. Conditions in the metamorphic Caledonides during the period of late orogenic cooling. Geological Magazine101, 457–65.CrossRefGoogle Scholar
Watson, J.1984. The ending of the Caledonian orogeny in Scotland. Journal of the Geological Society of London141, 193–214.CrossRefGoogle Scholar