Tab. 2: U-Pb ion-microprobe ages from Taymyr peninsula

We present the initial results of a U-Th-Pb zircon ion-microprobe investigation on samples from the Central Belt of Taimyr, in order to constrain its tectono-magmatic evolution. The zircon samples are from a deformed twomica granite (Faddey Massif), deformed metamorphosed gabbroic dike entrained as...

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Bibliographic Details
Main Authors: Pease, Victria, Vernikovsky, Valerij
Format: Dataset
Language:English
Published: PANGAEA 2000
Subjects:
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510
512
514
520
Age
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.759565
https://doi.org/10.1594/PANGAEA.759565