Edad de las terrazas y diques travertínicos de las Lagunas de Ruidera y sus implicaciones paleoclimáticas

J. Martínez Goytre; B. Hentzsch; F. López Vera; J. Martínez Frías

doi:10.3989/egeol.88441-2525

Edad de las terrazas y diques travertínicos de las Lagunas de Ruidera y sus implicaciones paleoclimáticas

Authors

J. Martínez Goytre Cátedra de Geodinámica. Facultad de Ciencias. Universidad Autónoma de Madrid
B. Hentzsch Instituto de Geología de Colonia
F. López Vera Cátedra de Geodinámica. Facultad de Ciencias. Universidad Autónoma de Madrid
J. Martínez Frías Dpto. de Geología. Museo Nacional de Ciencias Naturales (C.S.l.C.)

DOI:

https://doi.org/10.3989/egeol.88441-2525

Keywords:

Ruidera lates, terraces and sinter dykes, radiometric age, Paleoclimatology

Abstract

Two generations of carbonate sinter deposits of sedimentary origin occur along the shore line of the Ruidera lakes. Both of them were formed during interglaciar type climate conditions. Based on 234 U/238 U and 230 U/234 U activity relationships, two sets of ages were obtained: 10.000 years and 80.000-140.000; tbe former for the lower terraces and sinter dykes, the latter for the upper terraces.

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Published

1988-04-30

How to Cite

Martínez Goytre, J., Hentzsch, B., López Vera, F., & Martínez Frías, J. (1988). Edad de las terrazas y diques travertínicos de las Lagunas de Ruidera y sus implicaciones paleoclimáticas. Estudios Geológicos, 44(1-2), 75–81. https://doi.org/10.3989/egeol.88441-2525

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Issue

Vol. 44 No. 1-2 (1988)

Section

Articles

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