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Uranium-lead isotopic evidence from zircons for lower Palaeozoic tectonic activity in the Austroalpine Nappe, the Eastern Alps

✍ Scribed by R. A. Cliff


Book ID
104745552
Publisher
Springer
Year
1980
Tongue
English
Weight
776 KB
Volume
71
Category
Article
ISSN
0010-7999

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✦ Synopsis


U/Pb isotopic data for two zircon suites are presented :

(1) a pre D1 tonalite gneiss gives an age of 443 + 13 _ 16 m.y.

(2) a post D1 leucogranite gneiss gives 427+~ ~ m.y. Both zircon suites contain a minor inherited pre-Cambrian component. The data confirm a lower Palaeozoic age for the major, fabric-forming D~ event. Hercynian metamorphism which was sufficient to reset muscovite K/Ar ages to ca. 290 m.y. had little effect on the zircons. The possible importance of lower Palaeozoic orogeny in southern Europe and the uncertainties in regional palaeogeography are emphasised.