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Index Geophysics

Stratigraphy and paleomagnetism of the Esja, Eyrarfjall and Akrafjall Mountains, SW-Iceland

Item

Title (Dublin Core)

en-US Stratigraphy and paleomagnetism of the Esja, Eyrarfjall and Akrafjall Mountains, SW-Iceland

Description (Dublin Core)

en-US Detailed geological and magnetic mapping in an area of Pliocene and Plio-Pleistocene volcanic rocks in Southwestern Iceland has enabled us to correlate a 2,100-m-thick lava succession with similar dated sequences in Iceland and with the ocean-floor geomagnetic polarity time scale. This correlation, supported by additional K-Ar dating, implies (1) that the succession is between 4.2 and 1.8 Ma in age, (2) that at least 13 glaciations occurred in Western and Southwestern Iceland between 3.1 and 1.8 Ma ago, and (3) that at least two geomagnetic events are present in the Lower Matuyama epoch. Paleomagnetic results from 353 igneous units, mostly basalt lavas, are tabulated. Analysis of directions from 258 of these shows them to possess some serial correlation; their mean is very close to a central axial dipole field value, but explanations are proposed for observed systematic departures from this field in other Icelandic paleomagnetic survey results.
          ARK: https://n2t.net/ark:/88439/y042132
Permalink: https://geophysicsjournal.com/article/184
 

Creator (Dublin Core)

Kristjansson, L.
Fridleifsson, I.B.
Watkins, N.D.

Subject (Dublin Core)

en-US Paleomagnetism
en-US Basalt lavas
en-US Stratigraphy
en-US Glaciations
en-US Geomagnetic time scale
en-US Iceland
en-US Data

Publisher (Dublin Core)

en-US Journal of Geophysics

Date (Dublin Core)

1980-01-24

Type (Dublin Core)

info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
en-US Peer-reviewed Article

Format (Dublin Core)

application/pdf

Identifier (Dublin Core)

https://journal.geophysicsjournal.com/JofG/article/view/184

Source (Dublin Core)

en-US Journal of Geophysics; Vol 47 No 1 (1980): Journal of Geophysics; 31-42
2643-2986
2643-9271

Language (Dublin Core)

eng

Relation (Dublin Core)

https://journal.geophysicsjournal.com/JofG/article/view/184/144