Abstract:
Palaeomagnetic data from 15 hand samples collected in a sequence of tuffs of Carboniferous age (Andacollo Series) exposed in western Argentina (37°10′S, 70°38′W) are given. These samples show hydrothermal alteration. After AF and thermal cleaning the majority of samples show reversed polarity and yield a palaeomagnetic pole at 73.6°S, 64.7°E (dψ = 6°, dχ = 9°). By comparing the position of this pole with the apparent polar wander curve recognized for the Late Palaeozoic and Mesozoic of South America, quantitative support for a Cretaceous age for the cleaned remanence of these samples is given. K-Ar dating of the Andacollo rocks indicates a mean age of 69 ± 4 m.y.; this suggests that the isotopic system of these rocks became closed in Late Cretaceous time. Palaeomagnetic and radiometric data agree indicating a Cretaceous age for the hydrothermal alteration of the Andacollo rocks. © 1978.
Referencias:
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Citas:
---------- APA ----------
Vilas, J.F. & Valencio, D.A.
(1978)
. Palaeomagnetism and K-Ar dating of the Carboniferous Andacollo Series (Argentina) and the age of its hydrothermal overprinting. Earth and Planetary Science Letters, 40(1), 101-106.
http://dx.doi.org/10.1016/0012-821X(78)90078-X---------- CHICAGO ----------
Vilas, J.F., Valencio, D.A.
"Palaeomagnetism and K-Ar dating of the Carboniferous Andacollo Series (Argentina) and the age of its hydrothermal overprinting"
. Earth and Planetary Science Letters 40, no. 1
(1978) : 101-106.
http://dx.doi.org/10.1016/0012-821X(78)90078-X---------- MLA ----------
Vilas, J.F., Valencio, D.A.
"Palaeomagnetism and K-Ar dating of the Carboniferous Andacollo Series (Argentina) and the age of its hydrothermal overprinting"
. Earth and Planetary Science Letters, vol. 40, no. 1, 1978, pp. 101-106.
http://dx.doi.org/10.1016/0012-821X(78)90078-X---------- VANCOUVER ----------
Vilas, J.F., Valencio, D.A. Palaeomagnetism and K-Ar dating of the Carboniferous Andacollo Series (Argentina) and the age of its hydrothermal overprinting. Earth Plan. Sci. Lett. 1978;40(1):101-106.
http://dx.doi.org/10.1016/0012-821X(78)90078-X