Jökull


Jökull - 01.12.2006, Page 72

Jökull - 01.12.2006, Page 72
David W. McGarvie et al. Figure 6. Zn versus Nb, Y, and Sr variation diagram. The seven large filled symbols represent the five Ar-Ar dated samples plus the two most recent Holocene rhyolite eruptions at Torfa- jökull (data from McGarvie, 1985). Small open symbols for Nb and Sr are from an additional dataset of 23 analy- ses of Pleistocene rhyolites from Torfa- jökull (D.W. McGarvie, unpubl. data). Zn is used to trace changes in the liq- uid composition as Zn is consistently incompatible in Torfajökull rhyolites (McGarvie et al., 1990; Macdonald et al., 1990). – Hlutfall Zn, Nb, Y og Sr í 30 súrum bergsýnum af Torfajökuls- svæðinu. Figure 7. Age versus Zn, Nb, Y, and Sr. The five new analyses are plotted along with tie-lines between the data points to emphasise relationships. The sharp step from 83 ka to the 72/67 ka ring- fracture rhyolites is particularly pro- nounced for Zn, Nb, and Y, but less so for Sr due to feldspar variability (see Figure 5). Also shown are data from the two most recent Holocene rhyo- lite eruptions at Torfajökull (data from McGarvie, 1985), that emphasise the less-evolved character of recent rhy- olitic compositions erupted at Torfa- jökull. – Breytingar á hlutfalli Zn, Nb, Y og Sr með aldri í 7 súrum bergsýnum af Torfajökulssvæðinu. ements between the three oldest compositions span- ning the 384–83 ka period show near-linear trends; and third, between 83 ka and 71.4 ka , a pronounced change occurs that is marked by a sudden decrease in the concentrations of the incompatible elements (and a less convincing increase in Sr). It is important to note that the latter two trends are only revealed when examined in a stratigraphic context. The potential sig- nificance of these trends is now discussed. The first trend, from older and more-evolved to younger and less-evolved rhyolites at Torfajökull, confirms earlier work by McGarvie et al., (1990), and also by Ívarsson (1992) who showed that the compo- sitions of older rhyolites were always more-evolved than those of the Holocene rhyolites. The second trend, which shows a near-linear trend between the three dated samples from 384 ka to 83 ka (Figure 7), may only show strong linearity because of the small 70 JÖKULL No. 56
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