The Proterozoic evolution of northern Siberian Craton margin: a comparison of U–Pb–Hf signatures from sedimentary units of the Taimyr orogenic belt and the Siberian platform-Reference-Cited by-同舟云学术

The Proterozoic evolution of northern Siberian Craton margin: a comparison of U–Pb–Hf signatures from sedimentary units of the Taimyr orogenic belt and the Siberian platform

Published:2017-03-06 Issue:13 Volume:59 Page:1632-1656
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Priyatkina Nadezhda¹,Collins William J.¹²,Khudoley Andrei³,Zastrozhnov Dmitry⁴⁵,Ershova Victoria³,Chamberlain Kevin⁶⁷,Shatsillo Andrey⁸,Proskurnin Vasily⁴

Affiliation:

1. New South Wales Institute of Frontiers Geoscience, University of Newcastle, Newcastle, NSW, Australia

2. Department of Applied Geology, Curtin University, Perth, WA, Australia

3. Institute of the Earth Sciences, St. Petersburg State University, St. Petersburg, Russia

4. All Russian Geological Research Institute (VSEGEI), St. Petersburg, Russia

5. Centre for Earth Evolution and Dynamics (CEED), University of Oslo, Oslo, Norway

6. Department of Geology and Geophysics, University of Wyoming, Laramie, WY, USA

7. Faculty of Geology and Geography, Tomsk State University, Tomsk, Russia

8. Laboratory of Main Magnetic Field and Paleomagnetism, Institute of the Earth Physics (IFZ RAN), Moscow, Russia

Funder

Australian Research Council

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2017.1289341

Reference113 articles.

1. Insights on the crustal evolution of the West African Craton from Hf isotopes in detrital zircons from the Anti-Atlas belt

2. Late Proterozoic–Paleozoic evolution of the Arctic Alaska–Chukotka terrane based on U-Pb igneous and detrital zircon ages: Implications for Neoproterozoic paleogeographic reconstructions

3. Extinction of Cloudina and Namacalathus at the Precambrian-Cambrian boundary in Oman

4. Formation and Evolution of the Continental Crust

5. Use and abuse of crust-formation ages

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