Abstract:
The available palaeomagnetic-radiometric data close to the Matuyama-Gauss polarity transition are discussed. It is suggested that a change in the polarity of the geomagnetic field occurred between 2.20 and 2.31 my. It can be representative either of the Matuyama-Gauss polarity transition or of a normal polarity event. The available paleomagnetic-radiometric data support the first of these possibilities and the sea-floor spreading data the second one. © 1970.
Referencias:
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Citas:
---------- APA ----------
Valencio, D.A., Linares, E. & Vilas, J.F.
(1970)
. On the age of the Matuyama-Gauss transition. Earth and Planetary Science Letters, 8(2), 179-182.
http://dx.doi.org/10.1016/0012-821X(70)90170-6---------- CHICAGO ----------
Valencio, D.A., Linares, E., Vilas, J.F.
"On the age of the Matuyama-Gauss transition"
. Earth and Planetary Science Letters 8, no. 2
(1970) : 179-182.
http://dx.doi.org/10.1016/0012-821X(70)90170-6---------- MLA ----------
Valencio, D.A., Linares, E., Vilas, J.F.
"On the age of the Matuyama-Gauss transition"
. Earth and Planetary Science Letters, vol. 8, no. 2, 1970, pp. 179-182.
http://dx.doi.org/10.1016/0012-821X(70)90170-6---------- VANCOUVER ----------
Valencio, D.A., Linares, E., Vilas, J.F. On the age of the Matuyama-Gauss transition. Earth Plan. Sci. Lett. 1970;8(2):179-182.
http://dx.doi.org/10.1016/0012-821X(70)90170-6