|
Late Quaternary eruptions in Iceland |
The University of Plymouth, Department of Geographical Sciences, Drake Circus, Plymouth PL4 8AA, UK
1 University of Wales, Institute of Geology and Earth Studies, Llandinan Building, Aberystwyth SY23 3DB, UK
This paper assesses the potential of discriminant function analysis (DFA) for tephrochronology in the UK and Ireland. Current identification and correlation of Holocene tephras relies largely on radiocarbon dating to suggest a likely candidate eruption followed by a geochemical comparison using binary and ternary plots of selected major oxides. As more tephras are discovered, and the patterns of deposition appear increasingly complex, this approach is likely to work less effectively. In addition, the utility of tephra for the establishment of chronozones will be limited by the availability of radiometric dates to constrain the initial candidate eruption. The results of a DFA on some of the limited published geochemical data are presented and it is clear that this statistical technique offers advantages to the application and development of tephrochronology in western Europe. Future work should concentrate on the provision of discriminant functions from a more complete reference dataset, which will enable the identification of unknown tephras with a known probability of misclassification.
This article has been cited by other articles:
![]() |
R. A. Dodgshon, D. D. Gilbertson, and J. P. Grattan Endemic stress, farming communities and the influence of Icelandic volcanic eruptions in the Scottish Highlands Geological Society, London, Special Publications, 2000; 171: 267 - 280. [Abstract] [PDF] |
||||