Late Neoproterozoic evolution of the southwestern margin of the Siberian Craton: evidence from sedimentology, geochronology and detrital zircon analysis-Reference-Cited by-同舟云学术

Late Neoproterozoic evolution of the southwestern margin of the Siberian Craton: evidence from sedimentology, geochronology and detrital zircon analysis

Published:2020-07-10 Issue:13 Volume:63 Page:1658-1681
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Romanov Mikhail¹^ORCID,Sovetov Julius K.²³,Vernikovsky Valery A.²³,Rosenbaum Gideon¹^ORCID,Wilde Simon A.⁴,Vernikovskaya Antonina E.²³,Matushkin Nikolay Yu.²³,Kadilnikov Pavel I.²³

Affiliation:

1. School of Earth and Environmental Sciences, The University of Queensland, Brisbane, Australia

2. Trofimuk Institute of Petroleum Geology and Geophysics, SB RAS, Novosibirsk, Russia

3. Department of Geology and Geophysics, Novosibirsk State University, Novosibirsk, Russia

4. School of Earth and Planetary Sciences, Curtin University, Perth, Australia

Funder

an Australian Postgraduate Award (APA) from the University of Queensland

Russian Foundation for Basic Research

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2020.1790044

Reference104 articles.

1. Berzin, N.A., 1967, Main Fault Zone in the East Sayan (in Russian).: Moscow, Nauka, 147 p.

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