http://www.cnr.it/ontology/cnr/individuo/prodotto/ID181054
U-Pb SHRIMP zircon dating of andesite from the Dolomite area (NE Italy): geochronological evidence for the early onset of Permian Volcanism in the eastern part of the southern Alps (Articolo in rivista)
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- Label
- U-Pb SHRIMP zircon dating of andesite from the Dolomite area (NE Italy): geochronological evidence for the early onset of Permian Volcanism in the eastern part of the southern Alps (Articolo in rivista) (literal)
- Anno
- 2007-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s00015-007-1219-z (literal)
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- VISONÀ D; FIORETTI AM; POLI E; ZANFERRARI A; FANNING M (literal)
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- Rivista
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- Google Scholar (literal)
- ISI Web of Science (WOS) (literal)
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- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- 1 Dipartimento di Mineralogia e Petrologia, Universita', corso Garibaldi 37, 35137 Padova, Italy. E-mail: dario.visona@unipd.it
2 CNR - Istituto di Geoscienze e Georisorse, c.so Garibaldi 37, 35137 Padova, Italy
3 Dipartimento di Georisorse e Territorio, Università di Udine, via del Cotonificio 144, I-33100 Udine, Italy
4 Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia (literal)
- Titolo
- U-Pb SHRIMP zircon dating of andesite from the Dolomite area (NE Italy): geochronological evidence for the early onset of Permian Volcanism in the eastern part of the southern Alps (literal)
- Abstract
- The Athesian Volcanic District (AVD), a thick sequence of andesitic to rhyolitic
lava and ignimbrite, overlies both the Variscan basement of the
Dolomites and, where present, the continental basal conglomerate of Upper
Carboniferous(?) to Early Permian age. This volcanic activity is known to
mark the margin of the intra-Pangea megashear system between Gondwana
and Laurasia, the onset age of which is determined in this study.
SHRIMP U-Pb dating on zircon from Ponte Gardena/Waidbruck (Isarco/Eisack
valley) basaltic andesite yields an age of 290.7 ± 3 Ma, providing the oldest
record of andesite volcanic activity yet documented in the AVD. Two
younger dates (279.9 ± 3.3 and 278.6 ± 3.1 Ma) obtained for the andesitic necks
of M. dei Ginepri (Eores/Aferer valley) and Col Quaternà (western Comelico),
respectively, probably represent a second pulse of andesite magmatic activity.
Near Chiusa/Klausen, the volcanoclastic deposits at the bottom of the
Funes/Villnöss valley volcano-sedimentary complex only contain detrital zircons,
dated at 469 ± 6 Ma; these probably derive from erosion of Paleozoic
porphyroids. Other zircons from the same sediments and inherited cores of
magmatic andesite crystals give Paleoproterozoic (1953.6 ± 22.1, 1834.6 ± 69.3,
1773.6 ± 25.1 Ma), Early Neoproterozoic (1015 ± 14 Ma) and Late Neoproterozoic
(728.4 ± 9.6, 687.6 ± 7.6 Ma) ages. These ancient detrital and inherited
zircon ages fit the model that envisages the Dolomite region as being tectonically
coherent with Africa, at least until the Lower Permian. (literal)
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