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Science 4 October 1968:
Vol. 162. no. 3849, pp. 121 - 122
DOI: 10.1126/science.162.3849.121

Articles

Guatemela: Preliminary Zircon Ages from Central Cordillera

David N. Gomberg 1, Philip O. Banks 1, and Alexander R. McBirney 2

1 Department of Geology, Case Western Reserve University, Cleveland, Ohio
2 Department of Geology, University of Oregon, Eugene

Concordia resolution of uranium-lead analyses of zircons from rocks of the Guatemalan Cordillera indicates a period of plutonism, and perhaps metamorphism, in late Paleozoic times (345 ± 20 million years). Gneisses of the Chuacus Series yield an age of 1075 ± 25 million years which may be either the age of a source terrain for the original sediments, or the age of principal metamorphism. Zircons from a Paleozoic granite intruding the gneisses appear to contain inherited or contaminating material acquired during the process of magma generation or emplacement, or both.


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