Tephrochronology by microprobe glass analysis.

G. Larsen

doi:10.1007/978-94-009-8537-7_6

Tephrochronology by microprobe glass analysis.

G. Larsen

Engineering and Natural Sciences

University of Iceland

Research output: Contribution to journal › Article › peer-review

Abstract

Basaltic tephra layers form a considerable part of the postglacial tephra deposits in Iceland. Microprobe analysis of volcanic glass shards have made it possible to relate even very thin (1-2mm) basaltic tephra layers in distal areas outside the volcanic zones to their source.-from Author

Original language	English
Pages (from-to)	95-102
Number of pages	8
Journal	Tephra studies
DOIs	https://doi.org/10.1007/978-94-009-8537-7_6
Publication status	Published - 1981

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title = "Tephrochronology by microprobe glass analysis.",

abstract = "Basaltic tephra layers form a considerable part of the postglacial tephra deposits in Iceland. Microprobe analysis of volcanic glass shards have made it possible to relate even very thin (1-2mm) basaltic tephra layers in distal areas outside the volcanic zones to their source.-from Author",

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AB - Basaltic tephra layers form a considerable part of the postglacial tephra deposits in Iceland. Microprobe analysis of volcanic glass shards have made it possible to relate even very thin (1-2mm) basaltic tephra layers in distal areas outside the volcanic zones to their source.-from Author

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DO - 10.1007/978-94-009-8537-7_6

M3 - Article

SP - 95

EP - 102

JO - Tephra studies

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ER -

Tephrochronology by microprobe glass analysis.

Abstract

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