Paleomagnetic study of Deception Island, South Shetland Islands, Antarctica

Details Paleomagnetic study of Deception Island, South Shetland Islands, Antarctica Paleomagnetic study of Deception Island, South Shetland Islands, Antarctica

May 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003geoji.153..333b&link_type=abstract

Geophysical Journal International, Volume 153, Issue 2, pp. 333-343.

Astronomy and Astrophysics

Astronomy

4

Antarctica, Deception Island, Earth Magnetic Field, Palaeomagnetism, Palaeosecular Variation, Quaternary

Scientific paper

A paleomagnetic study was carried out on recent volcanic rocks exposed on Deception Island (63.0°S, 60.6°W), Antarctica. Sampling comprised all stratigraphic units exposed on the island, which include basaltic, andesitic and trachytic lavas, basaltic dykes and pyroclastic flows. Following stepwise thermal and alternating field demagnetization procedures, consistent characteristic remanence directions were determined at 21 sites, using principal-component analysis. The overall mean remanence direction for the Deception Island rocks is dec. 348.8°, inc. -73.7°, α95= 4.4°, N= 21, and is consistent within error with the geocentric axial dipole direction at the study locality. All of the studied rocks show normal polarity, indicating a Brunhes Chron age. The only available radiometric date of 153 +/- 46 kyr agrees with this and suggests a minimum chronostratigraphic span of 100 kyr for the sampled rocks. The site mean directions show a Fisherian distribution and dispersion values compatible with current palaeosecular variation models. No evidence of the far-sided or right-handed effect is found in our data.

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