Late Pleistocene geomagnetic excursion in Icelandic lavas: confirmation of the Laschamp excursion

Details Late Pleistocene geomagnetic excursion in Icelandic lavas: confirmation of the Laschamp excursion Late Pleistocene geomagnetic excursion in Icelandic lavas: confirmation of the Laschamp excursion

Jan 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990e%26psl..96..443l&link_type=abstract

Earth and Planetary Science Letters, Volume 96, Issue 3-4, p. 443-457.

Computer Science

56

Scientific paper

In 1980 Kristjansson and Gudmundsson [1] reported a late glacial geomagnetic excursion in three hills in the Reykjanes peninsula, Iceland, with shallow negative inclinations and westerly declinations. They named it the Skalamaelifell excursion. More extensive field work has identified the same excursional paleomagnetic direction (declination = 258°, inclination = -15°) at four additional outcrops in a 10 × 10 km area in the Reykjanes peninsula. The excursion lavas are olivine tholeiites with similar petrography and chemical compositions. Paleointensity determinations by the Thellier method average 4.2 +/- 0.2 μT for 8 samples, more than an order of magnitude weaker than the present geomagnetic field in Iceland. Together, these results suggest extrusion of the excursion lavas in a very brief span of time, probably less than a few hundred years.
K-Ar dating of the excursion lavas gives a mean age for 19 determinations of 42.9 +/- 7.8 ka (2σ). Compilation of thirty K-Ar ages of the Laschamp and Olby flows by three laboratories yield a new age for the Laschamp excursion in France of 46.6 +/- 2.4 ka (2σ). The age of the excursion in southwestern Iceland is statistically indistinguishable from the Laschamp excursion at the 95% confidence level, and both have very low paleointensities. Therefore, we suggest that the Laschamp and Olby flows in France and the Skalamaelifell units of Iceland recorded essentially the same geomagnetic excursion. Differences in the virtual paleomagnetic poles (VGPs) of these excursions may be due to (1) the probable non-dipole character of the geomagnetic field during the excursion, (2) rapid geomagnetic secular variation and possible small age differences of the extrusive rocks in France and Iceland, and/or (3) crustal magnetic anomalies which might dominate the local geomagnetic field during the excursion at either or both locations.

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