Jökull

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Jökull - 01.01.2017, Qupperneq 26

Jökull - 01.01.2017, Qupperneq 26
Holocene lavas in Bárðardalur, NE-Iceland Figure 3. Bárðardalur val- ley and the region north of Vatnajökull: (a) Bárð- ardalshraun lava following the Skjálfandafljót river to- wards the north. (b) Patch of the Kinnarhraun lava northwest of lake Svartár- vatn. (c) The Bárðardals- hraun lava with the Trölla- dyngja shield volcano in the background. – Ljósmyndir af hraunum í Bárðardal og norðan Vatnajökuls. plagioclase macrocrysts, is presented in a compan- ion paper. The rock samples include newly collected samples (B15–1 to B15–16) and a single archive sam- ple (NAL664) from the sample collection of the In- stitute of Earth Sciences, University of Iceland. Our sample selection includes different parts of the large Kinnarhraun and Bárðardalshraun lava flows (Fig- ure 3), the prehistoric Útbruni and Kvíahraun lavas, as well as the historical Frambruni lava. The sam- ples were taken from interiors of larger blocks to minimize surface weathering effects. The samples are generally relatively fresh and unaltered. How- ever, for some of the lava flows, especially Kinnar- hraun and Bárðardalshraun lavas, fresh samples were rare and most samples have somewhat prominent al- teration features, such as visible signs of oxidation (e.g., sample B15–10). Archive samples from base- ment rocks and nunataks of the Bárðarbunga cen- tral volcano, and the region north of Vatnajökull (i.e., Dyngjuháls, Urðarháls, Gígöldur, and Hrímalda) were also included in this study. Additional sample details can be found in Svavarsdóttir (2017). ANALYTICAL TECHNIQUES Inductively Coupled Plasma Optical Emission- Spectroscopy (ICP-OES) Major, minor and selected trace element analyses were acquired for all samples of this study (Table 1). The analyses were carried out with an ICP-OES in- strument (SPECTRO-CIROS) at the Institute of Earth JÖKULL No. 67, 2017 21
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