Geochronological evidence for late-Grenvillian magmatic and metamorphic events in central Taimyr, northern Siberia

U–Th–Pb analyses of zircons from six granites and one metasediment collected in the accretionary Central belt of Taimyr, Arctic Siberia, demonstrate that Neoproterozoic (c. 900 Ma) granites intrude late Mesoproterozoic/early Neoproterozoic amphibolite facies metamorphic rocks. This is the first time...

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Veröffentlicht in:	Terra nova (Oxford, England) England), 2001-08, Vol.13 (4), p.270-280
Hauptverfasser:	Pease, V., Gee, D. G., Vernikovsky, V., Vernikovskaya, A., Kireev, S.
Format:	Artikel
Sprache:	eng
Online-Zugang:	Volltext
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