Published July 1998
| public
Journal Article
Generation of Icelandic rhyolites: silicic lavas from the Torfajökull central volcano
Abstract
The Torfajökull central volcano in south-central Iceland contains the largest volume of exposed silicic extrusives in Iceland (∼225 km^3). Within SW-Torfajökull, postglacial mildly alkalic to peralkalic silicic lavas and lava domes (67–74 wt.% SiO_2) have erupted from a family of fissures 1–2.5 km apart within or just outside a large caldera (12×18 km). The silicic lavas show a fissure-dependent variation in composition, and form five chemically distinct units. The lavas are of low crystallinity (0–7 vol.%) and contain phenocrysts in the following order of decreasing abundance: plagioclase (An_(10-40)), Na-rich anorthoclase (
Additional Information
© 1998 Elsevier Science B.V. Received 17 April 1997; accepted 5 January 1998. We are grateful to Ole Stecher and Richard Carlson at the Department of Terrestrial Magnetism, Carnegie Institute for Sr and Nd-isotope analysis on the Torfajökull samples. We much appreciate insightful reviews by Tanya Furman, Sigurdur Steinthorsson, and Fergus Gibb. B.G. would like to thank Maria-Victoria Gunnarsson for her encouragement and valuable help in writing the initial draft of this paper as well as the initial drafting of many of the figures. Funding for this project came from the American Scandinavian Foundation to Bjorn Gunnarsson and the National Science Foundation grants EAR 86-18202, EAR 88-1734, and OPP 9418513 to Bruce Marsh and grants EAR 90-19190 and EAR 93-17036 to Hugh Taylor.Additional details
- Eprint ID
- 38364
- DOI
- 10.1016/S0377-0273(98)00017-1
- Resolver ID
- CaltechAUTHORS:20130508-142342503
- American Scandinavian Foundation
- EAR 86-18202
- NSF
- EAR 88-1734
- NSF
- OPP 9418513
- NSF
- EAR 90-19190
- NSF
- EAR 93-17036
- NSF
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2013-05-08Created from EPrint's datestamp field
- Updated
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2021-11-09Created from EPrint's last_modified field