Tephrochronology by Microprobe Glass Analysis
Basaltic tephra layers form a considerable part of the postglacial tephra deposits in Iceland. They can be related to the volcanic systems that produced them by characteristics based on major and minor element chemistry. Microprobe analysis of volcanic glass shards have made it possible to relate even very thin (1–2 mm) basaltic tephra layers in distal areas outside the volcanic zones to their source.
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- 2.Thorarinsson, S.: 1967, The Eruption of Hekla 1947–48, I, Soc. Sci. Islandica, pp. 1–170.Google Scholar
- 3.Thorarinsson, S.: 1959, Acta Nat. Isl. 22, pp. 1–100.Google Scholar
- 4.Larsen, G.: 1978, B. Sc. hon. Thesis, University of Iceland, pp. 1–59 (mimeographed).Google Scholar
- 5.Larsen, G. and Thorarinsson, S.: 1977, Jokull 27, pp. 28–46.Google Scholar
- 6.Saemundsson, K.: 1978, Geol. Journ. Spec. Iss. 10, pp. 415–432.Google Scholar
- 7.Jakobsson, S.P.: 1979, Acta Nat. Isl. 26, pp. 1–103.Google Scholar
- 8.Oskarsson, N., et al.: 1979, Nord. Vole. Inst, and Science Inst. Report 79 05/79 16, University of Iceland, pp. 1–104.Google Scholar
- 9.Larsen, G.: in preparation.Google Scholar