The Matuyama-Brunhes transition recorded from Lake Tecopa sediments (California)

Details The Matuyama-Brunhes transition recorded from Lake Tecopa sediments (California) The Matuyama-Brunhes transition recorded from Lake Tecopa sediments (California)

Mar 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988e%26psl..87..463v&link_type=abstract

Earth and Planetary Science Letters, Volume 87, Issue 4, p. 463-472.

Computer Science

30

Scientific paper

The paleomagnetic record of the Matuyama-Brunhes reversal in the sediment of ancient lake Tecopa provided the first evidence that the geomagnetic field during transition is not dipolar.
We resampled the section to increase the time resolution of the record. Our new data show that the characteristic direction could not be completely isolated by AF demagnetization. The transitional directions obtained from thermal demagnetization are thus quite different from those of the previous study but the primary conclusion that the field was non-dipolar remains. The VGP paths lying close to the site longitude is consistent with an axisymmetric transition field.

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