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HETZEL, RALF, ROMER, ROLF L. (1999) U–Pb dating of the Verkniy Ufaley intrusion, middle Urals, Russia: a minimum age for subduction and amphibolite facies overprint of the East European continental margin. Geological Magazine, 136 (5) 593-597 doi:10.1017/s0016756899002976

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Reference TypeJournal (article/letter/editorial)
TitleU–Pb dating of the Verkniy Ufaley intrusion, middle Urals, Russia: a minimum age for subduction and amphibolite facies overprint of the East European continental margin
JournalGeological Magazine
AuthorsHETZEL, RALFAuthor
ROMER, ROLF L.Author
Year1999 (September)Volume136
Issue5
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756899002976Search in ResearchGate
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Mindat Ref. ID258189Long-form Identifiermindat:1:5:258189:1
GUID0
Full ReferenceHETZEL, RALF, ROMER, ROLF L. (1999) U–Pb dating of the Verkniy Ufaley intrusion, middle Urals, Russia: a minimum age for subduction and amphibolite facies overprint of the East European continental margin. Geological Magazine, 136 (5) 593-597 doi:10.1017/s0016756899002976
Plain TextHETZEL, RALF, ROMER, ROLF L. (1999) U–Pb dating of the Verkniy Ufaley intrusion, middle Urals, Russia: a minimum age for subduction and amphibolite facies overprint of the East European continental margin. Geological Magazine, 136 (5) 593-597 doi:10.1017/s0016756899002976
In(1999, September) Geological Magazine Vol. 136 (5) Cambridge University Press (CUP)
Abstract/NotesThe Palaeozoic Uralian orogen formed by accretion of
island arcs and microcontinents along the eastern margin of
the East European platform. In the middle Urals, a promontory
of the East European platform, the Ufaley Complex
experienced eclogite facies conditions followed by an amphibolite
facies overprint. The Verkniy Ufaley intrusion crosscuts
the amphibolite facies foliation in the East Ufaley
Complex and thus postdates the two metamorphic events. A
concordant U–Pb age of 316±1 Ma obtained on magmatic
titanite dates the intrusion of the pluton and provides a
minimum age for subduction and subsequent amphibolite
facies metamorphism of the East European continental
margin. Zircon yields discordant age data that reflect the
involvement of Proterozoic crustal sources.

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Sindern, Sven, Gerdes, Axel, Ronkin, Yuri L., Dziggel, Annika, Hetzel, Ralf, Schulte, Bernd Aloys (2012) Monazite stability, composition and geochronology as tracers of Paleoproterozoic events at the eastern margin of the East European Craton (Taratash complex, Middle Urals) Lithos, 132. 82-97 doi:10.1016/j.lithos.2011.11.017
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Romer, Rolf L., Lüders, Volker (2006) Direct dating of hydrothermal W mineralization: U–Pb age for hübnerite (MnWO4), Sweet Home Mine, Colorado. Geochimica et Cosmochimica Acta, 70 (18) 4725-4733 doi:10.1016/j.gca.2006.07.003
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